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. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. J 1 I L 100. 200. 300. 400. J 1 500. HOURS. (DEPTH 23 M 40. • 20. o CO 0. -20. •40.. ilULjUlJlll Uj . ?' I ! 1 H II I 0. 10c. ]0. 400. soo. HOURS. (DEPTH 32 M.l Figure 13. Observed current, total period (v-component). Running mean (*), average over 1 inert, period 29. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lop Stock Photo

RMRNKKYA–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. J 1 I L 100. 200. 300. 400. J 1 500. HOURS. (DEPTH 23 M 40. • 20. o CO 0. -20. •40.. ilULjUlJlll Uj . ?' I ! 1 H II I 0. 10c. ]0. 400. soo. HOURS. (DEPTH 32 M.l Figure 13. Observed current, total period (v-component). Running mean (*), average over 1 inert, period 29. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lop

. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 40. 20. (T) C ) -20. -MO. 40.. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School Stock Photo

RMRNCDNB–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 40. 20. (T) C ) -20. -MO. 40.. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

. The ecology of the benthic and endolithic communities of a rocky reef in the kelp beds off Del Monte Beach, Monterey, California.. Oceanography. V I/O CO 4J c o M •H ^ O EC •» CO JJ o <u CO C CO u Eh <iH O C O •H +3 CO O o a hO C •H ^ O ^ CO cd . (D CO i:H ^ 5p:: 'O =5 (D ^ hO CO S^ CO (D J x: -p CJ CO J-. C T3 CO CO r-i 3 Q- O' in w a: o M 31. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Hoffman, Richard Gurney Stock Photo

RMRDY17T–. The ecology of the benthic and endolithic communities of a rocky reef in the kelp beds off Del Monte Beach, Monterey, California.. Oceanography. V I/O CO 4J c o M •H ^ O EC •» CO JJ o <u CO C CO u Eh <iH O C O •H +3 CO O o a hO C •H ^ O ^ CO cd . (D CO i:H ^ 5p:: 'O =5 (D ^ hO CO S^ CO (D J x: -p CJ CO J-. C T3 CO CO r-i 3 Q- O' in w a: o M 31. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Hoffman, Richard Gurney

. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o < o z o I— < D Lu Z o u z < o a o LU a z o 2 u o Q. bJ a o Id o z o < Ld ^— U o < J LU J J on < < LU CO lu < LU q: i/0. Figure 3.13 Streamlines at 37.5 m depth in the Kuroshio Current region for experiment 1. Streamlines are everywhere tangent to the current vectors and are selectively originated/discontinued to maintain neat-uniform spacing. 57. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability Stock Photo

RMRNTWJ9–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o < o z o I— < D Lu Z o u z < o a o LU a z o 2 u o Q. bJ a o Id o z o < Ld ^— U o < J LU J J on < < LU CO lu < LU q: i/0. Figure 3.13 Streamlines at 37.5 m depth in the Kuroshio Current region for experiment 1. Streamlines are everywhere tangent to the current vectors and are selectively originated/discontinued to maintain neat-uniform spacing. 57. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability

. A comparison of satellite images capable of detecting ocean surface features.. Oceanography. (a) (b) Figure 3. DMSP Standard Archived Products, 15 March 1973. (a) Portion of a high resolution visual image of the California coast. (b) Portion of a high resolution infrared image of the California coast, showing the same area Both images were taken at the same time by the same sensor, the scanning radiometer (SR). Again notice the usefulness of the visual image for differentiating between the ocean and clouds. Received from the University of Wisconsin, Madison. 56. Please note that these images Stock Photo

RMREF79N–. A comparison of satellite images capable of detecting ocean surface features.. Oceanography. (a) (b) Figure 3. DMSP Standard Archived Products, 15 March 1973. (a) Portion of a high resolution visual image of the California coast. (b) Portion of a high resolution infrared image of the California coast, showing the same area Both images were taken at the same time by the same sensor, the scanning radiometer (SR). Again notice the usefulness of the visual image for differentiating between the ocean and clouds. Received from the University of Wisconsin, Madison. 56. Please note that these images

. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o z o < u o z z o < cr 3 O u. z o (J z < u o en o $ LU LU a o LU a LU z o 2 u o Q. *W -1 — c o LU 2 a: 3 LU H < 2 < LU — CU «— u S o z LU o < LU H <— u -J o < < J LU LJ —1 2 LU H O < < < u a. CU. 71 OT S> s n in :r> LO ? LO "j -O iv. CM ii ii Z X — — 3 u 3 CO 2 3 Figure 3.18 Potential temperature in °C at 37.5 m depth in the East Australian Current region for experiment 1. 62. Please note that these images are extracted from scanned page images that ma Stock Photo

RMRNY4D4–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o z o < u o z z o < cr 3 O u. z o (J z < u o en o $ LU LU a o LU a LU z o 2 u o Q. *W -1 — c o LU 2 a: 3 LU H < 2 < LU — CU «— u S o z LU o < LU H <— u -J o < < J LU LJ —1 2 LU H O < < < u a. CU. 71 OT S> s n in :r> LO ? LO "j -O iv. CM ii ii Z X — — 3 u 3 CO 2 3 Figure 3.18 Potential temperature in °C at 37.5 m depth in the East Australian Current region for experiment 1. 62. Please note that these images are extracted from scanned page images that ma

. An analysis of results of a high-resolution world ocean circulation model. Oceanography. CASEA 1001 ITCRATION 10001 pabaiici ocf»h ciiwatc uonci ipocui onf ocgrfc hopio ocfan configuration no :• V VELOCITY LEVEL I 2.50M MOE I50E 160E I 70E 180 170*. I40E 1S0E IfcOE A- ROBUST DIAGNOSTIC RUN LOMIUUH INItHVAL • 5 00 FltLO niN . -39 •» IVfi *t -W Dtfbl SCALE FACTOR . 1 00 FIELD M»» « 15.2 iwwe «8 00si CASCA 1001 ITCRATION 10001 PAAAJ I Fl OrFAN CI IMATT UOflFI (POCMI Our nfr.OfF WOOI O OCFAN rOMFIC.KOATION NO 7 L> VELOCITY LEVEL I 2.S0M I40E 1S0E I60E I 70E f80 I 70«r. Please note that these Stock Photo

RMRNWJG5–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. CASEA 1001 ITCRATION 10001 pabaiici ocf»h ciiwatc uonci ipocui onf ocgrfc hopio ocfan configuration no :• V VELOCITY LEVEL I 2.50M MOE I50E 160E I 70E 180 170*. I40E 1S0E IfcOE A- ROBUST DIAGNOSTIC RUN LOMIUUH INItHVAL • 5 00 FltLO niN . -39 •» IVfi *t -W Dtfbl SCALE FACTOR . 1 00 FIELD M»» « 15.2 iwwe «8 00si CASCA 1001 ITCRATION 10001 PAAAJ I Fl OrFAN CI IMATT UOflFI (POCMI Our nfr.OfF WOOI O OCFAN rOMFIC.KOATION NO 7 L> VELOCITY LEVEL I 2.S0M I40E 1S0E I60E I 70E f80 I 70«r. Please note that these

RMRNY50X–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o < o z o I— < D Lu Z o u z < o a o LU a z o 2 u o Q. bJ a o Id o z o < Ld ^— U o < J LU J J on < < LU CO lu < LU q: i/0. Figure 3.13 Streamlines at 37.5 m depth in the Kuroshio Current region for experiment 1. Streamlines are everywhere tangent to the current vectors and are selectively originated/discontinued to maintain neat-uniform spacing. 57. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability

$. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. Q CD 40. 20. 0. -20. •40.. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School Stock Photo$

RMRNNB06–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. Q CD 40. 20. 0. -20. •40.. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

. British and European butterflies and moths (Macrolepidoptera). Lepidoptera -- Great Britain; Lepidoptera -- Europe. PLATE VI.. I. Nemeobius lucina, la. Under side. 2. Apatura iris, 2a. Female, 2b. Under side, -"c. Larva, 2d. Pupa. 3, Limenitis sibylla. 3a. Under side, 3b. Larva, 3c. Pupa. British and European Butiirflies and Moths.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Kappel, August Wilhelm; Kirby, Willia Stock Photo

RMRH37EN–. British and European butterflies and moths (Macrolepidoptera). Lepidoptera -- Great Britain; Lepidoptera -- Europe. PLATE VI.. I. Nemeobius lucina, la. Under side. 2. Apatura iris, 2a. Female, 2b. Under side, -"c. Larva, 2d. Pupa. 3, Limenitis sibylla. 3a. Under side, 3b. Larva, 3c. Pupa. British and European Butiirflies and Moths.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Kappel, August Wilhelm; Kirby, Willia

. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o o z < h- O o < UJ u o a. o UJ UJ cr. 15 UJ Q UJ Z o 2 u o a o o UJ I— o -J h- U. LJ cr u LU J UJ o Lj z ^o < UJ u o <C UJ (/") < < 3 in u < UJ a: cm l-. Figure 3.14 Streamlines at 1542.5 m depth in the Kuroshio Current region for experiment 1. Streamlines are everywhere tangent to the current vectors and are selectively originated/discontinued to maintain near-uniform spacing. 58. Please note that these images are extracted from scanned page images that may have been digi Stock Photo

RMRNKX88–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o o z < h- O o < UJ u o a. o UJ UJ cr. 15 UJ Q UJ Z o 2 u o a o o UJ I— o -J h- U. LJ cr u LU J UJ o Lj z ^o < UJ u o <C UJ (/") < < 3 in u < UJ a: cm l-. Figure 3.14 Streamlines at 1542.5 m depth in the Kuroshio Current region for experiment 1. Streamlines are everywhere tangent to the current vectors and are selectively originated/discontinued to maintain near-uniform spacing. 58. Please note that these images are extracted from scanned page images that may have been digi

RMRNYFD9–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. Q CD 40. 20. 0. -20. •40.. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. i 100. 200. 300. 400. 500. HOURS. [DEPTH 11 M. 40. 20. Q O u en -20. ?40.. J 1 I L 100. 200. 300. 400. J 1 500. HOURS. (DEPTH 23 M 40. • 20. o CO 0. -20. •40.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School Stock Photo

RMRNB08T–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. i 100. 200. 300. 400. 500. HOURS. [DEPTH 11 M. 40. 20. Q O u en -20. ?40.. J 1 I L 100. 200. 300. 400. J 1 500. HOURS. (DEPTH 23 M 40. • 20. o CO 0. -20. •40.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. u U J cr i- o cj I X UJ az 0- r. o u I ;> ?u. lc.. 10. 5. - ,^A- 1^1. >.r O.UOO 0.Q2S 0.US0 0.0?S 0.10Q 0.1^5 0.150 0.17S TOTfiL PEfllOO-OEPTh 1IM. 30. r 20. 10. iVt-j uaC. ^i,i. a 0.000 0.025 O.OSO 0.075 0.100 0.125 0.ISO 0.175 TOTAL PEfllQD-QEPTH 23M. cr UJ cc 0 r o Figure 11 25. 20. IS. 10. 5. - L 1'U. 1 0.000 Q.Q2S 0.050 0.0/5 0.100 0.125 0.150 0.175 TOTAL PEFHUQ-OEPTH 32M. Power spectrum of observed current. Total period (v-component). « (Abscissa: c.p.h.; ordinate: (cm/s) ) Stock Photo

RMRNHAXG–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. u U J cr i- o cj I X UJ az 0- r. o u I ;> ?u. lc.. 10. 5. - ,^A- 1^1. >.r O.UOO 0.Q2S 0.US0 0.0?S 0.10Q 0.1^5 0.150 0.17S TOTfiL PEfllOO-OEPTh 1IM. 30. r 20. 10. iVt-j uaC. ^i,i. a 0.000 0.025 O.OSO 0.075 0.100 0.125 0.ISO 0.175 TOTAL PEfllQD-QEPTH 23M. cr UJ cc 0 r o Figure 11 25. 20. IS. 10. 5. - L 1'U. 1 0.000 Q.Q2S 0.050 0.0/5 0.100 0.125 0.150 0.175 TOTAL PEFHUQ-OEPTH 32M. Power spectrum of observed current. Total period (v-component). « (Abscissa: c.p.h.; ordinate: (cm/s) )

RMRNHMTE–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. Q CD 40. 20. 0. -20. •40.. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNFBGR–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. CASEA 1001 ITCRATION 10001 pabaiici ocf»h ciiwatc uonci ipocui onf ocgrfc hopio ocfan configuration no :• V VELOCITY LEVEL I 2.50M MOE I50E 160E I 70E 180 170*. I40E 1S0E IfcOE A- ROBUST DIAGNOSTIC RUN LOMIUUH INItHVAL • 5 00 FltLO niN . -39 •» IVfi *t -W Dtfbl SCALE FACTOR . 1 00 FIELD M»» « 15.2 iwwe «8 00si CASCA 1001 ITCRATION 10001 PAAAJ I Fl OrFAN CI IMATT UOflFI (POCMI Our nfr.OfF WOOI O OCFAN rOMFIC.KOATION NO 7 L> VELOCITY LEVEL I 2.S0M I40E 1S0E I60E I 70E f80 I 70«r. Please note that these

. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 5 'JO t/J S sa o in in n m 3 rr 5 S lO in IT n in —• — 5 o T i CM ii li z X —a eC 3 3 O 3 -; U"> < Q CD O cr s s s s D u h- Z i/) — o — 3 C ) 3 C/i U Figure 3.17 Potential temperature in °C at 37.5 m depth in the Drake Passage region for experiment 1. 61. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A. Stock Photo

RMRNW6J0–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 5 'JO t/J S sa o in in n m 3 rr 5 S lO in IT n in —• — 5 o T i CM ii li z X —a eC 3 3 O 3 -; U"> < Q CD O cr s s s s D u h- Z i/) — o — 3 C ) 3 C/i U Figure 3.17 Potential temperature in °C at 37.5 m depth in the Drake Passage region for experiment 1. 61. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.

. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. 400. 500. HOURS. (DEPTH 32 M Figure 12. Observed current, total period (.u-component). Running mean (*), average over 1 inert, period 28. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate Sch Stock Photo

RMRNC0AN–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. 400. 500. HOURS. (DEPTH 32 M Figure 12. Observed current, total period (.u-component). Running mean (*), average over 1 inert, period 28. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate Sch

$. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. i 100. 200. 300. 400. 500. HOURS. [DEPTH 11 M. 40. 20. Q O u en -20. ?40.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School Stock Photo$

RMRNH4HX–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. i 100. 200. 300. 400. 500. HOURS. [DEPTH 11 M. 40. 20. Q O u en -20. ?40.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

. An analytic model of observed small scale baroclinic currents in the Arctic Ocean.. Oceanography. 100 i- E a a 20 0 - 300 — Velocity (cni/ sec) 4 0 60 80. Figure 3. Vertical Distribution of Horizontal Velocities Measured bv Gait [1967]. 16. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Itkin, Richard Ivan.. Monterey, California: U. S. Naval Postgraduate School Stock Photo

RMRNWB1W–. An analytic model of observed small scale baroclinic currents in the Arctic Ocean.. Oceanography. 100 i- E a a 20 0 - 300 — Velocity (cni/ sec) 4 0 60 80. Figure 3. Vertical Distribution of Horizontal Velocities Measured bv Gait [1967]. 16. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Itkin, Richard Ivan.. Monterey, California: U. S. Naval Postgraduate School

RMRND5AC–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o < o z o I— < D Lu Z o u z < o a o LU a z o 2 u o Q. bJ a o Id o z o < Ld ^— U o < J LU J J on < < LU CO lu < LU q: i/0. Figure 3.13 Streamlines at 37.5 m depth in the Kuroshio Current region for experiment 1. Streamlines are everywhere tangent to the current vectors and are selectively originated/discontinued to maintain neat-uniform spacing. 57. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability

RMRNKXH0–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 5 'JO t/J S sa o in in n m 3 rr 5 S lO in IT n in —• — 5 o T i CM ii li z X —a eC 3 3 O 3 -; U"> < Q CD O cr s s s s D u h- Z i/) — o — 3 C ) 3 C/i U Figure 3.17 Potential temperature in °C at 37.5 m depth in the Drake Passage region for experiment 1. 61. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.

RMRNKW8H–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 40. 20. (T) C ) -20. -MO. 40.. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNXDCE–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. u U J cr i- o cj I X UJ az 0- r. o u I ;> ?u. lc.. 10. 5. - ,^A- 1^1. >.r O.UOO 0.Q2S 0.US0 0.0?S 0.10Q 0.1^5 0.150 0.17S TOTfiL PEfllOO-OEPTh 1IM. 30. r 20. 10. iVt-j uaC. ^i,i. a 0.000 0.025 O.OSO 0.075 0.100 0.125 0.ISO 0.175 TOTAL PEfllQD-QEPTH 23M. cr UJ cc 0 r o Figure 11 25. 20. IS. 10. 5. - L 1'U. 1 0.000 Q.Q2S 0.050 0.0/5 0.100 0.125 0.150 0.175 TOTAL PEFHUQ-OEPTH 32M. Power spectrum of observed current. Total period (v-component). « (Abscissa: c.p.h.; ordinate: (cm/s) )

RMRNCX7G–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. CASEA 1001 ITCRATION 10001 pabaiici ocf»h ciiwatc uonci ipocui onf ocgrfc hopio ocfan configuration no :• V VELOCITY LEVEL I 2.50M MOE I50E 160E I 70E 180 170*. I40E 1S0E IfcOE A- ROBUST DIAGNOSTIC RUN LOMIUUH INItHVAL • 5 00 FltLO niN . -39 •» IVfi *t -W Dtfbl SCALE FACTOR . 1 00 FIELD M»» « 15.2 iwwe «8 00si CASCA 1001 ITCRATION 10001 PAAAJ I Fl OrFAN CI IMATT UOflFI (POCMI Our nfr.OfF WOOI O OCFAN rOMFIC.KOATION NO 7 L> VELOCITY LEVEL I 2.S0M I40E 1S0E I60E I 70E f80 I 70«r. Please note that these

RMRNJFH7–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 5 'JO t/J S sa o in in n m 3 rr 5 S lO in IT n in —• — 5 o T i CM ii li z X —a eC 3 3 O 3 -; U"> < Q CD O cr s s s s D u h- Z i/) — o — 3 C ) 3 C/i U Figure 3.17 Potential temperature in °C at 37.5 m depth in the Drake Passage region for experiment 1. 61. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.

. An analysis of results of a high-resolution world ocean circulation model. Oceanography. . Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.. Monterey, California: U. S. Naval Postgraduate School Stock Photo

RMRNXX51–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. . Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.. Monterey, California: U. S. Naval Postgraduate School

RMRNY8AP–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o o z < h- O o < UJ u o a. o UJ UJ cr. 15 UJ Q UJ Z o 2 u o a o o UJ I— o -J h- U. LJ cr u LU J UJ o Lj z ^o < UJ u o <C UJ (/") < < 3 in u < UJ a: cm l-. Figure 3.14 Streamlines at 1542.5 m depth in the Kuroshio Current region for experiment 1. Streamlines are everywhere tangent to the current vectors and are selectively originated/discontinued to maintain near-uniform spacing. 58. Please note that these images are extracted from scanned page images that may have been digi

RMRP08A5–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o z o < u o z z o < cr 3 O u. z o (J z < u o en o $ LU LU a o LU a LU z o 2 u o Q. *W -1 — c o LU 2 a: 3 LU H < 2 < LU — CU «— u S o z LU o < LU H <— u -J o < < J LU LJ —1 2 LU H O < < < u a. CU. 71 OT S> s n in :r> LO ? LO "j -O iv. CM ii ii Z X — — 3 u 3 CO 2 3 Figure 3.18 Potential temperature in °C at 37.5 m depth in the East Australian Current region for experiment 1. 62. Please note that these images are extracted from scanned page images that ma

RMRNDA31–. An analytic model of observed small scale baroclinic currents in the Arctic Ocean.. Oceanography. 100 i- E a a 20 0 - 300 — Velocity (cni/ sec) 4 0 60 80. Figure 3. Vertical Distribution of Horizontal Velocities Measured bv Gait [1967]. 16. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Itkin, Richard Ivan.. Monterey, California: U. S. Naval Postgraduate School

RMRNH167–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 40. 20. (T) C ) -20. -MO. 40.. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNFW92–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. 400. 500. HOURS. (DEPTH 32 M Figure 12. Observed current, total period (.u-component). Running mean (*), average over 1 inert, period 28. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate Sch

RMRNWG3D–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. Q CD 40. 20. 0. -20. •40.. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNJGYK–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o o z < h- O o < UJ u o a. o UJ UJ cr. 15 UJ Q UJ Z o 2 u o a o o UJ I— o -J h- U. LJ cr u LU J UJ o Lj z ^o < UJ u o <C UJ (/") < < 3 in u < UJ a: cm l-. Figure 3.14 Streamlines at 1542.5 m depth in the Kuroshio Current region for experiment 1. Streamlines are everywhere tangent to the current vectors and are selectively originated/discontinued to maintain near-uniform spacing. 58. Please note that these images are extracted from scanned page images that may have been digi

. An analysis of results of a high-resolution world ocean circulation model. Oceanography. s s in m ifl T ?2- n" s s in m rr — re re s — — 3 OT Figure 3.15 Horizontal volume transport in Sv(=10-'-^ cnr s ) in the Drake Passage region for experiment 1. 59. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.. Monterey, California: U. S. Naval Postgraduate School Stock Photo

RMRNCX4N–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. s s in m ifl T ?2- n" s s in m rr — re re s — — 3 OT Figure 3.15 Horizontal volume transport in Sv(=10-'-^ cnr s ) in the Drake Passage region for experiment 1. 59. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.. Monterey, California: U. S. Naval Postgraduate School

RMRNYA42–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o < o z o I— < D Lu Z o u z < o a o LU a z o 2 u o Q. bJ a o Id o z o < Ld ^— U o < J LU J J on < < LU CO lu < LU q: i/0. Figure 3.13 Streamlines at 37.5 m depth in the Kuroshio Current region for experiment 1. Streamlines are everywhere tangent to the current vectors and are selectively originated/discontinued to maintain neat-uniform spacing. 57. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability

RMRNPP77–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 40. 20. (T) C ) -20. -MO. 40.. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNTKGW–. An analytic model of observed small scale baroclinic currents in the Arctic Ocean.. Oceanography. 100 i- E a a 20 0 - 300 — Velocity (cni/ sec) 4 0 60 80. Figure 3. Vertical Distribution of Horizontal Velocities Measured bv Gait [1967]. 16. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Itkin, Richard Ivan.. Monterey, California: U. S. Naval Postgraduate School

RMRNR9G3–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 5 'JO t/J S sa o in in n m 3 rr 5 S lO in IT n in —• — 5 o T i CM ii li z X —a eC 3 3 O 3 -; U"> < Q CD O cr s s s s D u h- Z i/) — o — 3 C ) 3 C/i U Figure 3.17 Potential temperature in °C at 37.5 m depth in the Drake Passage region for experiment 1. 61. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.

RMRNTC2G–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. u U J cr i- o cj I X UJ az 0- r. o u I ;> ?u. lc.. 10. 5. - ,^A- 1^1. >.r O.UOO 0.Q2S 0.US0 0.0?S 0.10Q 0.1^5 0.150 0.17S TOTfiL PEfllOO-OEPTh 1IM. 30. r 20. 10. iVt-j uaC. ^i,i. a 0.000 0.025 O.OSO 0.075 0.100 0.125 0.ISO 0.175 TOTAL PEfllQD-QEPTH 23M. cr UJ cc 0 r o Figure 11 25. 20. IS. 10. 5. - L 1'U. 1 0.000 Q.Q2S 0.050 0.0/5 0.100 0.125 0.150 0.175 TOTAL PEFHUQ-OEPTH 32M. Power spectrum of observed current. Total period (v-component). « (Abscissa: c.p.h.; ordinate: (cm/s) )

RMRNCPYM–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 5 'JO t/J S sa o in in n m 3 rr 5 S lO in IT n in —• — 5 o T i CM ii li z X —a eC 3 3 O 3 -; U"> < Q CD O cr s s s s D u h- Z i/) — o — 3 C ) 3 C/i U Figure 3.17 Potential temperature in °C at 37.5 m depth in the Drake Passage region for experiment 1. 61. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.

RMRNTH4X–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o o z < h- O o < UJ u o a. o UJ UJ cr. 15 UJ Q UJ Z o 2 u o a o o UJ I— o -J h- U. LJ cr u LU J UJ o Lj z ^o < UJ u o <C UJ (/") < < 3 in u < UJ a: cm l-. Figure 3.14 Streamlines at 1542.5 m depth in the Kuroshio Current region for experiment 1. Streamlines are everywhere tangent to the current vectors and are selectively originated/discontinued to maintain near-uniform spacing. 58. Please note that these images are extracted from scanned page images that may have been digi

RMRNWDJC–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. . Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.. Monterey, California: U. S. Naval Postgraduate School

RMRNEWMJ–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. i 100. 200. 300. 400. 500. HOURS. [DEPTH 11 M. 40. 20. Q O u en -20. ?40.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNC3XM–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. . Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.. Monterey, California: U. S. Naval Postgraduate School

RMRNDTR6–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. i 100. 200. 300. 400. 500. HOURS. [DEPTH 11 M. 40. 20. Q O u en -20. ?40.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNKC9F–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 5 'JO t/J S sa o in in n m 3 rr 5 S lO in IT n in —• — 5 o T i CM ii li z X —a eC 3 3 O 3 -; U"> < Q CD O cr s s s s D u h- Z i/) — o — 3 C ) 3 C/i U Figure 3.17 Potential temperature in °C at 37.5 m depth in the Drake Passage region for experiment 1. 61. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.

RMRNB412–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. i 100. 200. 300. 400. 500. HOURS. [DEPTH 11 M. 40. 20. Q O u en -20. ?40.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNF6HP–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o o z < h- O o < UJ u o a. o UJ UJ cr. 15 UJ Q UJ Z o 2 u o a o o UJ I— o -J h- U. LJ cr u LU J UJ o Lj z ^o < UJ u o <C UJ (/") < < 3 in u < UJ a: cm l-. Figure 3.14 Streamlines at 1542.5 m depth in the Kuroshio Current region for experiment 1. Streamlines are everywhere tangent to the current vectors and are selectively originated/discontinued to maintain near-uniform spacing. 58. Please note that these images are extracted from scanned page images that may have been digi

RMRNFB7N–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. u U J cr i- o cj I X UJ az 0- r. o u I ;> ?u. lc.. 10. 5. - ,^A- 1^1. >.r O.UOO 0.Q2S 0.US0 0.0?S 0.10Q 0.1^5 0.150 0.17S TOTfiL PEfllOO-OEPTh 1IM. 30. r 20. 10. iVt-j uaC. ^i,i. a 0.000 0.025 O.OSO 0.075 0.100 0.125 0.ISO 0.175 TOTAL PEfllQD-QEPTH 23M. cr UJ cc 0 r o Figure 11 25. 20. IS. 10. 5. - L 1'U. 1 0.000 Q.Q2S 0.050 0.0/5 0.100 0.125 0.150 0.175 TOTAL PEFHUQ-OEPTH 32M. Power spectrum of observed current. Total period (v-component). « (Abscissa: c.p.h.; ordinate: (cm/s) )

RMRNDA11–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 40. 20. (T) C ) -20. -MO. 40.. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNDJE9–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o o z < h- O o < UJ u o a. o UJ UJ cr. 15 UJ Q UJ Z o 2 u o a o o UJ I— o -J h- U. LJ cr u LU J UJ o Lj z ^o < UJ u o <C UJ (/") < < 3 in u < UJ a: cm l-. Figure 3.14 Streamlines at 1542.5 m depth in the Kuroshio Current region for experiment 1. Streamlines are everywhere tangent to the current vectors and are selectively originated/discontinued to maintain near-uniform spacing. 58. Please note that these images are extracted from scanned page images that may have been digi

RMRNCMG9–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. 400. 500. HOURS. (DEPTH 32 M Figure 12. Observed current, total period (.u-component). Running mean (*), average over 1 inert, period 28. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate Sch

RMRNXWHF–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. i 100. 200. 300. 400. 500. HOURS. [DEPTH 11 M. 40. 20. Q O u en -20. ?40.. J 1 I L 100. 200. 300. 400. J 1 500. HOURS. (DEPTH 23 M 40. • 20. o CO 0. -20. •40.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNDH4E–. An analytic model of observed small scale baroclinic currents in the Arctic Ocean.. Oceanography. 100 i- E a a 20 0 - 300 — Velocity (cni/ sec) 4 0 60 80. Figure 3. Vertical Distribution of Horizontal Velocities Measured bv Gait [1967]. 16. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Itkin, Richard Ivan.. Monterey, California: U. S. Naval Postgraduate School

RMRNXPJW–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. CASEA 1001 ITCRATION 10001 pabaiici ocf»h ciiwatc uonci ipocui onf ocgrfc hopio ocfan configuration no :• V VELOCITY LEVEL I 2.50M MOE I50E 160E I 70E 180 170*. I40E 1S0E IfcOE A- ROBUST DIAGNOSTIC RUN LOMIUUH INItHVAL • 5 00 FltLO niN . -39 •» IVfi *t -W Dtfbl SCALE FACTOR . 1 00 FIELD M»» « 15.2 iwwe «8 00si CASCA 1001 ITCRATION 10001 PAAAJ I Fl OrFAN CI IMATT UOflFI (POCMI Our nfr.OfF WOOI O OCFAN rOMFIC.KOATION NO 7 L> VELOCITY LEVEL I 2.S0M I40E 1S0E I60E I 70E f80 I 70«r. Please note that these

. A critical analysis of ocean thermal analysis models in operation at FNOC.. Oceanography. NPS-68-84-015 NAVAL POSTGRADUATE SCHOOL Monterey, California. THESIS A CRITICAL ANALYSIS OF OCEAN THERMAL ANALYSIS MODELS IN OPERATION AT FNOC by Brian James Brady September 1984 Thesis Advisor: C. N . K. Mooers Approved for public release, distribution unlimited Prepared for: Office of Naval Research Ocean Sciences and Technology Division (Code 422PO) Arlington, Virginia 22217 1217383. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readabi Stock Photo

RMRE5DNP–. A critical analysis of ocean thermal analysis models in operation at FNOC.. Oceanography. NPS-68-84-015 NAVAL POSTGRADUATE SCHOOL Monterey, California. THESIS A CRITICAL ANALYSIS OF OCEAN THERMAL ANALYSIS MODELS IN OPERATION AT FNOC by Brian James Brady September 1984 Thesis Advisor: C. N . K. Mooers Approved for public release, distribution unlimited Prepared for: Office of Naval Research Ocean Sciences and Technology Division (Code 422PO) Arlington, Virginia 22217 1217383. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readabi

. The book of bugs. The Way of the Mosquito. 51 quinine until his ears rung. There was a young man in my class in college so fond of the drug that he would dip it out of a big bottle on his % knife-blade and lick it off. He said it tasted good. It gave me the all-overs to watch him. They used to tell a story about a Hoosier going into a drug- store and asking the clerk for quinine. The clerk wanted to know it he would have it in capsules. ' Capsules ? W hat's cap- sules ? " The clerk showed him. " Right purty. What they fur?" To put the quinine in." " Whutch want t Stock Photo

RMRHDA3P–. The book of bugs. The Way of the Mosquito. 51 quinine until his ears rung. There was a young man in my class in college so fond of the drug that he would dip it out of a big bottle on his % knife-blade and lick it off. He said it tasted good. It gave me the all-overs to watch him. They used to tell a story about a Hoosier going into a drug- store and asking the clerk for quinine. The clerk wanted to know it he would have it in capsules. ' Capsules ? W hat's cap- sules ? " The clerk showed him. " Right purty. What they fur?" To put the quinine in." " Whutch want t

RMRNBY85–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. Q CD 40. 20. 0. -20. •40.. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNKCNY–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. s s in m ifl T ?2- n" s s in m rr — re re s — — 3 OT Figure 3.15 Horizontal volume transport in Sv(=10-'-^ cnr s ) in the Drake Passage region for experiment 1. 59. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.. Monterey, California: U. S. Naval Postgraduate School

RMRNNB9R–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. i 100. 200. 300. 400. 500. HOURS. [DEPTH 11 M. 40. 20. Q O u en -20. ?40.. J 1 I L 100. 200. 300. 400. J 1 500. HOURS. (DEPTH 23 M 40. • 20. o CO 0. -20. •40.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNFN8Y–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. i 100. 200. 300. 400. 500. HOURS. [DEPTH 11 M. 40. 20. Q O u en -20. ?40.. J 1 I L 100. 200. 300. 400. J 1 500. HOURS. (DEPTH 23 M 40. • 20. o CO 0. -20. •40.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNEKYN–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 5 'JO t/J S sa o in in n m 3 rr 5 S lO in IT n in —• — 5 o T i CM ii li z X —a eC 3 3 O 3 -; U"> < Q CD O cr s s s s D u h- Z i/) — o — 3 C ) 3 C/i U Figure 3.17 Potential temperature in °C at 37.5 m depth in the Drake Passage region for experiment 1. 61. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.

RMRNXK06–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o z o < u o z z o < cr 3 O u. z o (J z < u o en o $ LU LU a o LU a LU z o 2 u o Q. *W -1 — c o LU 2 a: 3 LU H < 2 < LU — CU «— u S o z LU o < LU H <— u -J o < < J LU LJ —1 2 LU H O < < < u a. CU. 71 OT S> s n in :r> LO ? LO "j -O iv. CM ii ii Z X — — 3 u 3 CO 2 3 Figure 3.18 Potential temperature in °C at 37.5 m depth in the East Australian Current region for experiment 1. 62. Please note that these images are extracted from scanned page images that ma

RMRNHR86–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. u U J cr i- o cj I X UJ az 0- r. o u I ;> ?u. lc.. 10. 5. - ,^A- 1^1. >.r O.UOO 0.Q2S 0.US0 0.0?S 0.10Q 0.1^5 0.150 0.17S TOTfiL PEfllOO-OEPTh 1IM. 30. r 20. 10. iVt-j uaC. ^i,i. a 0.000 0.025 O.OSO 0.075 0.100 0.125 0.ISO 0.175 TOTAL PEfllQD-QEPTH 23M. cr UJ cc 0 r o Figure 11 25. 20. IS. 10. 5. - L 1'U. 1 0.000 Q.Q2S 0.050 0.0/5 0.100 0.125 0.150 0.175 TOTAL PEFHUQ-OEPTH 32M. Power spectrum of observed current. Total period (v-component). « (Abscissa: c.p.h.; ordinate: (cm/s) )

. California range brushlands and browse plants. Browse (Animal food); Brush; Forage plants. Ceanothus lemmonii Ceanothus thyrsitlorns. Distribution of lemmon ceanothus (Ceanothus lemmonii) and blueblos- som ceanothus (Ceanothus thyrsiflorus). shrub, 1/2 to 3 feet high, with gray or whitish hairy branches and branchlets. Leaves alternate, eliptical, or oblong-elliptic, Yi inch to VA inches long, % to % inch wide, finely hairy to smooth, bright green and waxen above, paler and densely hairy beneath, margins usually glan- dular toothed. Flowers pale blue, in simple clusters, M inch to 1 inch lon Stock Photo

RMRG3H87–. California range brushlands and browse plants. Browse (Animal food); Brush; Forage plants. Ceanothus lemmonii Ceanothus thyrsitlorns. Distribution of lemmon ceanothus (Ceanothus lemmonii) and blueblos- som ceanothus (Ceanothus thyrsiflorus). shrub, 1/2 to 3 feet high, with gray or whitish hairy branches and branchlets. Leaves alternate, eliptical, or oblong-elliptic, Yi inch to VA inches long, % to % inch wide, finely hairy to smooth, bright green and waxen above, paler and densely hairy beneath, margins usually glan- dular toothed. Flowers pale blue, in simple clusters, M inch to 1 inch lon

RMRNN8TK–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. Q CD 40. 20. 0. -20. •40.. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNH6NH–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 40. 20. (T) C ) -20. -MO. 40.. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNMNB3–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. . Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.. Monterey, California: U. S. Naval Postgraduate School

RMRNTDG5–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o < o z o I— < D Lu Z o u z < o a o LU a z o 2 u o Q. bJ a o Id o z o < Ld ^— U o < J LU J J on < < LU CO lu < LU q: i/0. Figure 3.13 Streamlines at 37.5 m depth in the Kuroshio Current region for experiment 1. Streamlines are everywhere tangent to the current vectors and are selectively originated/discontinued to maintain neat-uniform spacing. 57. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability

RMRNGAAG–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 40. 20. (T) C ) -20. -MO. 40.. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNJPY4–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. 400. 500. HOURS. (DEPTH 32 M Figure 12. Observed current, total period (.u-component). Running mean (*), average over 1 inert, period 28. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate Sch

. The book of bugs. The Way of the Mosquito. 49. the mental process that is satisfied with that conclusion. It puzzles me. I declare I can't see for the life of me what there is that is so smart about it, and yet to hear them get it off you •-j - would think it ended the whole matter. Yhen you come t o look over the problem of malaria in the light of recent discovery, it seems strange we did not sooner find out its intimate connection with mosquitoes. People used to say of a place: There ought not to be any malaria there. It is good high ground, fine natural drainage, and far from any swamps. Stock Photo

RMRHDA3Y–. The book of bugs. The Way of the Mosquito. 49. the mental process that is satisfied with that conclusion. It puzzles me. I declare I can't see for the life of me what there is that is so smart about it, and yet to hear them get it off you •-j - would think it ended the whole matter. Yhen you come t o look over the problem of malaria in the light of recent discovery, it seems strange we did not sooner find out its intimate connection with mosquitoes. People used to say of a place: There ought not to be any malaria there. It is good high ground, fine natural drainage, and far from any swamps.

. Acoustical oceanography of the Levantine Sea.. Oceanography. ram <n.rx. ^ KS-'.v'v. Figure 27. Distribution of the clay-mineral assemblages in the eastern Mediterranean Sea; l=Nile assemblage; 2=southeast Aegean assemblage; 3=kaolinite-rich assemblage; 4=Kitnira assemblage (Venkatarathnam and Ryan, 1971],. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Cubukcu, Nazim. Monterey, California: U. S. Naval Postgraduate Sch Stock Photo

RMRR48TX–. Acoustical oceanography of the Levantine Sea.. Oceanography. ram <n.rx. ^ KS-'.v'v. Figure 27. Distribution of the clay-mineral assemblages in the eastern Mediterranean Sea; l=Nile assemblage; 2=southeast Aegean assemblage; 3=kaolinite-rich assemblage; 4=Kitnira assemblage (Venkatarathnam and Ryan, 1971],. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Cubukcu, Nazim. Monterey, California: U. S. Naval Postgraduate Sch

RMRNC92H–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 40. 20. (T) C ) -20. -MO. 40.. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

. California range brushlands and browse plants. Browse (Animal food); Brush; Forage plants. Distribution (map shown below). This species occu- pies dry warm habitats of the foothills and lower moun- tain slopes in various habitats, between 500 to 4,000 feet elevation, and often forms dense stands over extensive areas. It occurs in the Coast Ranges from northern San Luis Obispo County, northward to the Siskiyou Moun- tains, and in the Sierra Nevada foothills from Kern and Tulare counties northward to Plumas County; also in southern Oregon. Economic value. Mature California verba santa stands a Stock Photo

RMRG3XG3–. California range brushlands and browse plants. Browse (Animal food); Brush; Forage plants. Distribution (map shown below). This species occu- pies dry warm habitats of the foothills and lower moun- tain slopes in various habitats, between 500 to 4,000 feet elevation, and often forms dense stands over extensive areas. It occurs in the Coast Ranges from northern San Luis Obispo County, northward to the Siskiyou Moun- tains, and in the Sierra Nevada foothills from Kern and Tulare counties northward to Plumas County; also in southern Oregon. Economic value. Mature California verba santa stands a

. An atlas of Secchi disc transparency measurements and Forel-Ule color codes for the oceans of the world.. Oceanography. 0 w. 3 <9 i. I. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Frederick, Margaret Anne. Monterey, California: U. S. Naval Postgraduate School Stock Photo

RMRJYC7T–. An atlas of Secchi disc transparency measurements and Forel-Ule color codes for the oceans of the world.. Oceanography. 0 w. 3 <9 i. I. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Frederick, Margaret Anne. Monterey, California: U. S. Naval Postgraduate School

. Acoustical oceanography of the Levantine Sea.. Oceanography. > o +-> CL III T3 3 O 3 >> r— +J c •r- O Q. -)-> (tJ oo 01 O 00 01 •r— E c 03 s- en SS01 104. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Cubukcu, Nazim. Monterey, California: U. S. Naval Postgraduate School Stock Photo

RMRR48BH–. Acoustical oceanography of the Levantine Sea.. Oceanography. > o +-> CL III T3 3 O 3 >> r— +J c •r- O Q. -)-> (tJ oo 01 O 00 01 •r— E c 03 s- en SS01 104. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Cubukcu, Nazim. Monterey, California: U. S. Naval Postgraduate School

RMRNCMPE–. An analytic model of observed small scale baroclinic currents in the Arctic Ocean.. Oceanography. 100 i- E a a 20 0 - 300 — Velocity (cni/ sec) 4 0 60 80. Figure 3. Vertical Distribution of Horizontal Velocities Measured bv Gait [1967]. 16. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Itkin, Richard Ivan.. Monterey, California: U. S. Naval Postgraduate School

RMRNJAYY–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 40. 20. (T) C ) -20. -MO. 40.. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNDHKT–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. Q CD 40. 20. 0. -20. •40.. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNBTTX–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. i 100. 200. 300. 400. 500. HOURS. [DEPTH 11 M. 40. 20. Q O u en -20. ?40.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNMKWP–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 40. 20. (T) C ) -20. -MO. 40.. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNG82J–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. Q CD 40. 20. 0. -20. •40.. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNXMBX–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. CASEA 1001 ITCRATION 10001 pabaiici ocf»h ciiwatc uonci ipocui onf ocgrfc hopio ocfan configuration no :• V VELOCITY LEVEL I 2.50M MOE I50E 160E I 70E 180 170*. I40E 1S0E IfcOE A- ROBUST DIAGNOSTIC RUN LOMIUUH INItHVAL • 5 00 FltLO niN . -39 •» IVfi *t -W Dtfbl SCALE FACTOR . 1 00 FIELD M»» « 15.2 iwwe «8 00si CASCA 1001 ITCRATION 10001 PAAAJ I Fl OrFAN CI IMATT UOflFI (POCMI Our nfr.OfF WOOI O OCFAN rOMFIC.KOATION NO 7 L> VELOCITY LEVEL I 2.S0M I40E 1S0E I60E I 70E f80 I 70«r. Please note that these

. The effect of a single resonant expansion chamber on the propagation of long waves in a channel.. Oceanography. 1.0 37 T(sec) 20 17 15 13 12 cvi oc 0.5 0.0 1R= 150ft bR=300ft bM = 200ft TTTT. 0.2 0"0 0.6 CJ (rod/sec) SQUARE OF THE REFLECTION COEFFICIENT 75 CVI I 50[-n I 25 Ef=l8fr H,/, = 12 ft Tl/3=l2.7ft. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Hudspeth, Robert Turner.. University of Washington Stock Photo

RMRDFFK7–. The effect of a single resonant expansion chamber on the propagation of long waves in a channel.. Oceanography. 1.0 37 T(sec) 20 17 15 13 12 cvi oc 0.5 0.0 1R= 150ft bR=300ft bM = 200ft TTTT. 0.2 0"0 0.6 CJ (rod/sec) SQUARE OF THE REFLECTION COEFFICIENT 75 CVI I 50[-n I 25 Ef=l8fr H,/, = 12 ft Tl/3=l2.7ft. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Hudspeth, Robert Turner.. University of Washington

RMRND9DC–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. o o o o z < h- O o < UJ u o a. o UJ UJ cr. 15 UJ Q UJ Z o 2 u o a o o UJ I— o -J h- U. LJ cr u LU J UJ o Lj z ^o < UJ u o <C UJ (/") < < 3 in u < UJ a: cm l-. Figure 3.14 Streamlines at 1542.5 m depth in the Kuroshio Current region for experiment 1. Streamlines are everywhere tangent to the current vectors and are selectively originated/discontinued to maintain near-uniform spacing. 58. Please note that these images are extracted from scanned page images that may have been digi

RMRNXDGW–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 40. 20. (T) C ) -20. -MO. 40.. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

RMRNBBE2–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. u U J cr i- o cj I X UJ az 0- r. o u I ;> ?u. lc.. 10. 5. - ,^A- 1^1. >.r O.UOO 0.Q2S 0.US0 0.0?S 0.10Q 0.1^5 0.150 0.17S TOTfiL PEfllOO-OEPTh 1IM. 30. r 20. 10. iVt-j uaC. ^i,i. a 0.000 0.025 O.OSO 0.075 0.100 0.125 0.ISO 0.175 TOTAL PEfllQD-QEPTH 23M. cr UJ cc 0 r o Figure 11 25. 20. IS. 10. 5. - L 1'U. 1 0.000 Q.Q2S 0.050 0.0/5 0.100 0.125 0.150 0.175 TOTAL PEFHUQ-OEPTH 32M. Power spectrum of observed current. Total period (v-component). « (Abscissa: c.p.h.; ordinate: (cm/s) )

RMRNTW1F–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. . Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.. Monterey, California: U. S. Naval Postgraduate School

RMRNN3J2–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 5 'JO t/J S sa o in in n m 3 rr 5 S lO in IT n in —• — 5 o T i CM ii li z X —a eC 3 3 O 3 -; U"> < Q CD O cr s s s s D u h- Z i/) — o — 3 C ) 3 C/i U Figure 3.17 Potential temperature in °C at 37.5 m depth in the Drake Passage region for experiment 1. 61. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.

RMRNH6F4–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. . Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.. Monterey, California: U. S. Naval Postgraduate School

RMRNH7MA–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. . Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.. Monterey, California: U. S. Naval Postgraduate School

. Acoustic fluctuations due to shallow thermal microstructure.. Oceanography. > CO z: UJ CD CE CT LJ UJ CO ' CD D Run ix. 0.99 r jj E. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Hagen, James Burgess.. Monterey, California: U. S. Naval Postgraduate School Stock Photo

RMRR48CA–. Acoustic fluctuations due to shallow thermal microstructure.. Oceanography. > CO z: UJ CD CE CT LJ UJ CO ' CD D Run ix. 0.99 r jj E. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Hagen, James Burgess.. Monterey, California: U. S. Naval Postgraduate School

RMRNJRWH–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. 100. 200. 300. 400. HOURS. (DEPTH 11 M.) 1 i i 500. 500.. 400. 500. HOURS. (DEPTH 32 M Figure 12. Observed current, total period (.u-component). Running mean (*), average over 1 inert, period 28. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate Sch

. A critical analysis of ocean thermal analysis models in operation at FNOC.. Oceanography. 0 100 c. Difference Field 30 Jun. d. TEOTS Analysis 7 Jul e toe e. Difference Field 7 Jul Figure 5.16 Contoured THG Fields for TEOTS/Cruise All (contour units oc/1000) . 82. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Brady, Brian J.. Monterey, California: U. S. Naval Postgraduate School Stock Photo

RMRE5DA6–. A critical analysis of ocean thermal analysis models in operation at FNOC.. Oceanography. 0 100 c. Difference Field 30 Jun. d. TEOTS Analysis 7 Jul e toe e. Difference Field 7 Jul Figure 5.16 Contoured THG Fields for TEOTS/Cruise All (contour units oc/1000) . 82. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Brady, Brian J.. Monterey, California: U. S. Naval Postgraduate School

RMRNDMKK–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. Q CD 40. 20. 0. -20. •40.. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

. Cnoidal wave theory applied to radiation stress phenomena.. Oceanography. Figure 1 Cnoidal Wave o— Experim e n ta I Wave (after Taylor, 1955) Solitary Wave Sinusoidal Wave. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Musick, George Meredith. Monterey, California: U. S. Naval Postgraduate School Stock Photo

RMREK5GJ–. Cnoidal wave theory applied to radiation stress phenomena.. Oceanography. Figure 1 Cnoidal Wave o— Experim e n ta I Wave (after Taylor, 1955) Solitary Wave Sinusoidal Wave. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Musick, George Meredith. Monterey, California: U. S. Naval Postgraduate School

RMRNPA66–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 5 'JO t/J S sa o in in n m 3 rr 5 S lO in IT n in —• — 5 o T i CM ii li z X —a eC 3 3 O 3 -; U"> < Q CD O cr s s s s D u h- Z i/) — o — 3 C ) 3 C/i U Figure 3.17 Potential temperature in °C at 37.5 m depth in the Drake Passage region for experiment 1. 61. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Barton, Wesley A.

RMRNN992–. Analysis and simulation of wind-driven currents during the Mixed Layer Experiment (MILE).. Oceanography. Q CD 40. 20. 0. -20. •40.. h U C, n. R A^T!! •/''ill I ?'{'* •?,' ' n. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lopez, Jose M. Fernandez. Monterey, California: U. S. Naval Postgraduate School

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