Salinity model hi-res stock photography and images

Brachionus plicatilis, Print, Brachionus plicatilis is a euryhaline (tolerate a wide range of salinity) rotifer in the Family Brachionidae, and is possibly the only commercially important rotifer, being raised in the aquaculture industry as food for fish larvae. It has a broad distribution in salt lakes around the world and has become a model system for studies in ecology and evolution Stock Photo

RM2A2M3MK–Brachionus plicatilis, Print, Brachionus plicatilis is a euryhaline (tolerate a wide range of salinity) rotifer in the Family Brachionidae, and is possibly the only commercially important rotifer, being raised in the aquaculture industry as food for fish larvae. It has a broad distribution in salt lakes around the world and has become a model system for studies in ecology and evolution

Elementary science teacher discusses salinity in class model released Stock Photo

RMA0AB38–Elementary science teacher discusses salinity in class model released

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RMH428RP–Senegal, Lac rose, salt production, worker, Africa, West, Africa, Lac Retba, economy, waters, water, lake, salt lake, salinity, salt, salty, boots, people, salt fishermen, man, Senegalese, dark-skinned, drying, shovel, yield,

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Doctor in respirator show a virus model. Slow motion. Woman wearing protect medical aerosol spray paint mask. Green ball spike thorn. Stock Photo

RF2BB4BMR–Doctor in respirator show a virus model. Slow motion. Woman wearing protect medical aerosol spray paint mask. Green ball spike thorn.

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RFERFG49–Permil 3d golden sign isolated on white background

RM2AY9G4B–Permil 3D golden sign

A boy who has just applied therapeutic mud of the Salinas and Arenales of San Pedro del Pinatar, Spain Stock Photo

RFJC0CFA–A boy who has just applied therapeutic mud of the Salinas and Arenales of San Pedro del Pinatar, Spain

. An analytic model of observed small scale baroclinic currents in the Arctic Ocean.. Oceanography. 2800 Figure 7. Observations of Salinity, Temperature and Density Taken Under Ice Island T-3. 2 2. 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

RMRNAK1H–. An analytic model of observed small scale baroclinic currents in the Arctic Ocean.. Oceanography. 2800 Figure 7. Observations of Salinity, Temperature and Density Taken Under Ice Island T-3. 2 2. 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

. Development of a microcomputer coupled Atmospheric and Oceanic Boundary Layer prediction model.. Meteorology; Oceanography. Retreat Mode Compute Updated: Mixed layer depth Well mixed temperature (SST) Well mixed salinity. 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.. Tarbet, Gary Lee.. Monterey, California: U. S. Naval Postgraduate School Stock Photo

RMPFA7Y3–. Development of a microcomputer coupled Atmospheric and Oceanic Boundary Layer prediction model.. Meteorology; Oceanography. Retreat Mode Compute Updated: Mixed layer depth Well mixed temperature (SST) Well mixed salinity. 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.. Tarbet, Gary Lee.. Monterey, California: U. S. Naval Postgraduate School

RMMAAED1–. The ecology of the Apalachicola Bay system : an estuarine profile . INCREASED MICROBIAL BIOMASS TIDAL SUBSIDY WIND DISTURBANCE II PHB/LIPIDS '"COj RELEASE Oj UTILIZATION y BASE, DETRITAL FOOD WEBS Figure 25. Tentative model of microbial interactions with various physical and biological processes in the Apalachicola River estuary (Livingston 1983c). dissolved nutrients into a shallow bay ecosystem characterized by gradients of salinity is seen to provide the appro- priate components for a highly productive system. Tidal and wind-induced currents, periodic flooding, and predation all prov

Doctor in respirator show a virus model concept health safety protection coronavirus epidemic 2019 nCoV. Slow motion. Woman wearing protect medical ae Stock Photo

RF2HPA69D–Doctor in respirator show a virus model concept health safety protection coronavirus epidemic 2019 nCoV. Slow motion. Woman wearing protect medical ae

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RFJC0CPY–Result of applying mud bath throughout the body

. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography Periodicals.. 312 J. F. Festa & D. V. Hansen. Figure i. An idealized estuarine system. fresher as the river transport increases. The estuarine circulation becomes stronger for increasing Rayleigh numbeis. Consequently internal dynamics determine seaward boundary profiles as well as those within the estuary. The boundary conditions given at the seaward end of the model must be consistent with these internal dynamics. Thus, salinity and velocity profiles cannot Stock Photo

RMREGWFA–. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography Periodicals.. 312 J. F. Festa & D. V. Hansen. Figure i. An idealized estuarine system. fresher as the river transport increases. The estuarine circulation becomes stronger for increasing Rayleigh numbeis. Consequently internal dynamics determine seaward boundary profiles as well as those within the estuary. The boundary conditions given at the seaward end of the model must be consistent with these internal dynamics. Thus, salinity and velocity profiles cannot

. Development of a microcomputer coupled Atmospheric and Oceanic Boundary Layer prediction model.. Meteorology; Oceanography. Prescribed Inputs: Surface wind speed and direction Incident Radiation Precipitation - Evaporation Surface (lm) Radiation Absorption Critical Richardson Number N/ Required Profiles: Temperature Salinity Velocity Compute: Surface Fluxes Stability Parameters. 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 wo Stock Photo

RMPFA7Y8–. Development of a microcomputer coupled Atmospheric and Oceanic Boundary Layer prediction model.. Meteorology; Oceanography. Prescribed Inputs: Surface wind speed and direction Incident Radiation Precipitation - Evaporation Surface (lm) Radiation Absorption Critical Richardson Number N/ Required Profiles: Temperature Salinity Velocity Compute: Surface Fluxes Stability Parameters. 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 wo

. The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder . I Figure 32-10. Distribution of Pacific herring in October and the relationship of adults (mature) and juveniles (immature) to salinity gradients. (Modified from Rumyant- sevand Darda 1970.) have been made to estimate herring biomass by a Soviet hydroacoustic trawl survey, ecosystem model- ing, and aerial surveys of spawning biomass. In 1963, three years after the fishery began, the eastern Bering Sea herring biomass was estimated to be 2.16 million mt, based on a Soviet hydroacoustic su Stock Photo

RMMAA303–. The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder . I Figure 32-10. Distribution of Pacific herring in October and the relationship of adults (mature) and juveniles (immature) to salinity gradients. (Modified from Rumyant- sevand Darda 1970.) have been made to estimate herring biomass by a Soviet hydroacoustic trawl survey, ecosystem model- ing, and aerial surveys of spawning biomass. In 1963, three years after the fishery began, the eastern Bering Sea herring biomass was estimated to be 2.16 million mt, based on a Soviet hydroacoustic su

Applying hand bath therapeutic mud of Mar Menor in Spain Stock Photo

RFJC0CMR–Applying hand bath therapeutic mud of Mar Menor in Spain

RMREH21D–. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography Periodicals.. Passive Microwave Detection 22-33 PACIFIC OCEAN. Figure 22.31 Average distribution of sea-surface salinity for the Pacific Ocean in parts per thousand (after Muromtsev, 1963). 22.2.4.2 Foam The emissivity of foam is much higher than that of the sea surface. This was first suggested by Williams (1969) based on experimental data, and was supported theoretically on the basis of a physical model for foam by Droppleman (1970). Recent experimental data, r

RMPFA7XR–. Development of a microcomputer coupled Atmospheric and Oceanic Boundary Layer prediction model.. Meteorology; Oceanography. Retreat Mode Compute Updated: Mixed layer depth Well mixed temperature (SST) Well mixed salinity. Figure 5. Input and Flow Chart for CBL Prediction Model 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.. Tarbet, Gary Lee.. Monterey, California: U. S. Naval Postgraduate School

Close-up of a boy after applying a therapeutic mud bath in San Pedro del Pinatar, Spain Stock Photo

RFJC5D56–Close-up of a boy after applying a therapeutic mud bath in San Pedro del Pinatar, Spain

. Coastal hydraulic models. Hydraulic models. MAXIMUM AND MINIMUM SALINITY MEASUREMENTS DELAWARE MEMORIAL BRIDGE, CHESTER AND FORT MIFFLIN MIDOEPTH-MEAN TIDE, 1965 HYOROGRAPH Figure 3-34. Verification of long-term salinity conditions, Delaware River model (after Simmons, Harrison, and Huval, 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.. Hudson, Robert Y. Fort Belvoir, Va. : U. S. Coastal Engineering Research Cente Stock Photo

RMREK244–. Coastal hydraulic models. Hydraulic models. MAXIMUM AND MINIMUM SALINITY MEASUREMENTS DELAWARE MEMORIAL BRIDGE, CHESTER AND FORT MIFFLIN MIDOEPTH-MEAN TIDE, 1965 HYOROGRAPH Figure 3-34. Verification of long-term salinity conditions, Delaware River model (after Simmons, Harrison, and Huval, 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.. Hudson, Robert Y. Fort Belvoir, Va. : U. S. Coastal Engineering Research Cente

. The Biological bulletin. Biology; Zoology; Biology; Marine Biology. 1 § .5. O Veligers • Embryos Control Gradual Abrupt Hours Figure 3. Model predictions of Melanochlamys diomedea egg-mass salinity as a function of time at three internal positions. The egg mass was assumed to be spherical with radius a = 0.566 cm. At the beginning of the simulation the salinity was 30%r throughout the egg mass. The external salinity was held constant at 5%c. Salinity treatment Figure 5. Survival of degelled embryos (•) and veligers (D) of Melanochlamv.i diomedea subjected to gradual or abrupt salinity change Stock Photo

RMRHM986–. The Biological bulletin. Biology; Zoology; Biology; Marine Biology. 1 § .5. O Veligers • Embryos Control Gradual Abrupt Hours Figure 3. Model predictions of Melanochlamys diomedea egg-mass salinity as a function of time at three internal positions. The egg mass was assumed to be spherical with radius a = 0.566 cm. At the beginning of the simulation the salinity was 30%r throughout the egg mass. The external salinity was held constant at 5%c. Salinity treatment Figure 5. Survival of degelled embryos (•) and veligers (D) of Melanochlamv.i diomedea subjected to gradual or abrupt salinity change

. The Biological bulletin. Biology; Zoology; Biology; Marine Biology. 78 C. P. MANGUM AND J. S. RAINER and seaside crabs are responsible for the differences in Hc02 affinity. Because Hc02 affinity also changes with season (Mauro and Mangum, 1982), we performed our experiments during July—the same month in which pre- vious experiments were performed (Mason et ai, 1983). Materials and Methods We either captured or purchased crabs from local wa- termen whose pots had been placed at known locations. Water salinity was determined, by conductivity (Yellow Springs Instrument Co. Model 33 salinometer) Stock Photo

RMRHN2E3–. The Biological bulletin. Biology; Zoology; Biology; Marine Biology. 78 C. P. MANGUM AND J. S. RAINER and seaside crabs are responsible for the differences in Hc02 affinity. Because Hc02 affinity also changes with season (Mauro and Mangum, 1982), we performed our experiments during July—the same month in which pre- vious experiments were performed (Mason et ai, 1983). Materials and Methods We either captured or purchased crabs from local wa- termen whose pots had been placed at known locations. Water salinity was determined, by conductivity (Yellow Springs Instrument Co. Model 33 salinometer)

RMREGTM8–. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography Periodicals.. ZONt OF WIND-OHVEN SMOAiiNG DOWNWELUNO WAVES COASTAL JET ng 1. Hypothetical model of the coastal boundary of the storm flow field during a period of onshore wind. Convergence of wind driven current with shoreline results in downwelling coastal jet. salinity stratification. During such storms, wind stress on the sea surface drives Langmuir circula- tion in the mixed layer (Gordon and Gerard, in press). The stratified lower layer is eroded by this mec

RMREGWDT–. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography Periodicals.. Two-dimensional circulation model 319 distance over which 5^o-i5%0 at the bottom of the estuary, is a strong function of fresh- water discharge. It increases from 44 km for Uf = 4 cm/s to 170 km for U( = 0-5 cm/s as shown in Figures 5 and 6. This behavior has been empirically, if qualitatively, known to hydraulic engineers for many years. The functional form of the dependence of salinity intrusion upon freshwater discharge is of special interest bec

RMREGTMX–. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography Periodicals.. cfhelf Sedimentation 119 SUI'ACI WINO OIIVIN CUIIINI • OTTO** WIND OftlVEN CUIIEHI SUtFACE WAVI DI1VCN CUItENT. ZONt OF WIND-OHVEN SMOAiiNG DOWNWELUNO WAVES COASTAL JET ng 1. Hypothetical model of the coastal boundary of the storm flow field during a period of onshore wind. Convergence of wind driven current with shoreline results in downwelling coastal jet. salinity stratification. During such storms, wind stress on the sea surface drives Langmuir

. Coast watch. Marine resources; Oceanography; Coastal zone management; Coastal ecology. ments will also be conducted to monitor the effects of salinity func- tions on growth rates. —Ken Reckhow from Duke Univer- sity's School of Forestry and Environ- mental Studies will combine the research models into an overall model for the project. Project manager Dave Adams says the drainage problem is complex, but a start must be made towards a solution. Adams, visiting associate professor with NCSU's Department of Forestry and University Studies, says that the study's "tangible product will be a r Stock Photo

RMREK3N6–. Coast watch. Marine resources; Oceanography; Coastal zone management; Coastal ecology. ments will also be conducted to monitor the effects of salinity func- tions on growth rates. —Ken Reckhow from Duke Univer- sity's School of Forestry and Environ- mental Studies will combine the research models into an overall model for the project. Project manager Dave Adams says the drainage problem is complex, but a start must be made towards a solution. Adams, visiting associate professor with NCSU's Department of Forestry and University Studies, says that the study's "tangible product will be a r

. The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder. Oceanography Bering Sea.. Pacific herring 519. I Figure 32-10. Distribution of Pacific herring in October and the relationship of adults (mature) and juveniles (immature) to salinity gradients. (Modified from Rumyant- sevand Darda 1970.) have been made to estimate herring biomass by a Soviet hydroacoustic trawl survey, ecosystem model- ing, and aerial surveys of spawning biomass. In 1963, three years after the fishery began, the eastern Bering Sea herring biomass was estimated to be 2.16 Stock Photo

RMRE5AGR–. The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder. Oceanography Bering Sea.. Pacific herring 519. I Figure 32-10. Distribution of Pacific herring in October and the relationship of adults (mature) and juveniles (immature) to salinity gradients. (Modified from Rumyant- sevand Darda 1970.) have been made to estimate herring biomass by a Soviet hydroacoustic trawl survey, ecosystem model- ing, and aerial surveys of spawning biomass. In 1963, three years after the fishery began, the eastern Bering Sea herring biomass was estimated to be 2.16

. The Biological bulletin. Biology; Zoology; Biology; Marine Biology. 172 CHARLES M. FUSS, JR. AND LARRY H. OGREN substrate-water interface with an Ekman-Merz type meter before and after the release of each five shrimp. Salinity was determined by a density hydrometer or recorded continuously with an Industrial Instruments/Minneapolis-Honeywell single point strip chart salinity recorder-indicator2 having a CELVH10270 conductivity cell. Incident light was recorded in situ or on the surface with a SeaTec model 210 Low Level Light DATE (1964) -FEB 20 6 - SUNSET. WEATHER CLEAR SHRIMP SIZE I30-140mm Stock Photo

RMRHNRRN–. The Biological bulletin. Biology; Zoology; Biology; Marine Biology. 172 CHARLES M. FUSS, JR. AND LARRY H. OGREN substrate-water interface with an Ekman-Merz type meter before and after the release of each five shrimp. Salinity was determined by a density hydrometer or recorded continuously with an Industrial Instruments/Minneapolis-Honeywell single point strip chart salinity recorder-indicator2 having a CELVH10270 conductivity cell. Incident light was recorded in situ or on the surface with a SeaTec model 210 Low Level Light DATE (1964) -FEB 20 6 - SUNSET. WEATHER CLEAR SHRIMP SIZE I30-140mm

. Coastal hydraulic models. Hydraulic models. O VELOCITY AND SALINITY STATION ,—e VELOCITY AND SALINITY RANGE (PROTOTYPE) B -. = =.— -- SHOALING SECTION IC L: . — EXISTING CONDITIONS BASE TEST-26-ft CHANNEL SCALES IN FEET CHANNEL LAYOUT MODEL TEST DATA (T 25 TIDE 3-4 AUGUST 1968 FRESHWATER DISCHARGE 10,000 ft^/s "source SALINITY 32 PPT. 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.. Hudson, Robert Y. Fort Belvoir, Va. Stock Photo

RMREK22P–. Coastal hydraulic models. Hydraulic models. O VELOCITY AND SALINITY STATION ,—e VELOCITY AND SALINITY RANGE (PROTOTYPE) B -. = =.— -- SHOALING SECTION IC L: . — EXISTING CONDITIONS BASE TEST-26-ft CHANNEL SCALES IN FEET CHANNEL LAYOUT MODEL TEST DATA (T 25 TIDE 3-4 AUGUST 1968 FRESHWATER DISCHARGE 10,000 ft^/s "source SALINITY 32 PPT. 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.. Hudson, Robert Y. Fort Belvoir, Va.

. Coastal hydraulic models. Hydraulic models. ATLANTIC ScEAN LOCATION OF VELOCITY AND SALINITY STATIONS ji AND TIDE GAGES / SCALE IN FEET HEAD BAY PROTOTYPE 'Â°ra â â J â Â°auÂ»itfÂ°Â° MODEL '!^ â i - Figure 3-6. Savannah Harbor model (after U.S. Army Engineer Waterways Experiment Station, 1961). 69. 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.. Hudson, Robert Y. Fort Belvoir, Va. : U. S. Coastal Engineering Research Cent Stock Photo

RMREJH84–. Coastal hydraulic models. Hydraulic models. ATLANTIC ScEAN LOCATION OF VELOCITY AND SALINITY STATIONS ji AND TIDE GAGES / SCALE IN FEET HEAD BAY PROTOTYPE 'Â°ra â â J â Â°auÂ»itfÂ°Â° MODEL '!^ â i - Figure 3-6. Savannah Harbor model (after U.S. Army Engineer Waterways Experiment Station, 1961). 69. 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.. Hudson, Robert Y. Fort Belvoir, Va. : U. S. Coastal Engineering Research Cent

. BOMEX temporary archive description of available data Terry De La Moriniere. Oceanography Research Atlantic Ocean.. 5.4 kHz Discriminator SCARD PLAYBACK UNIT (SPEED= I 7/8 IPS) AMR B- TO "REALTIME" TO CYCLE COUNTERS FOR DIGITIZING. SKL 302 (2 SECTIONS USED) CD FILTERED AND £! SHAPED DEPTH t Q or o FILTERED AND SHAPED Ll TEMPERATURE rr UJ ERED AND SHAPED o SALINITY UJ ) o > o FILTERED AND SHAPED DEPTH DANA MODEL 2200s (over-driven by TEKTRONIX 555amps) o h- Figure 1-13. Separation and signal conditioning of the recorded signal prior to input for digitization. 110. Please note th Stock Photo

RMRHE604–. BOMEX temporary archive description of available data Terry De La Moriniere. Oceanography Research Atlantic Ocean.. 5.4 kHz Discriminator SCARD PLAYBACK UNIT (SPEED= I 7/8 IPS) AMR B- TO "REALTIME" TO CYCLE COUNTERS FOR DIGITIZING. SKL 302 (2 SECTIONS USED) CD FILTERED AND £! SHAPED DEPTH t Q or o FILTERED AND SHAPED Ll TEMPERATURE rr UJ ERED AND SHAPED o SALINITY UJ ) o > o FILTERED AND SHAPED DEPTH DANA MODEL 2200s (over-driven by TEKTRONIX 555amps) o h- Figure 1-13. Separation and signal conditioning of the recorded signal prior to input for digitization. 110. Please note th

RMREK22D–. Coastal hydraulic models. Hydraulic models. O VELOCITY AND SALINITY STATION ,—e VELOCITY AND SALINITY RANGE (PROTOTYPE) B -. = =.— -- SHOALING SECTION IC L: . — EXISTING CONDITIONS BASE TEST-26-ft CHANNEL SCALES IN FEET CHANNEL LAYOUT MODEL TEST DATA (T 25 TIDE 3-4 AUGUST 1968 FRESHWATER DISCHARGE 10,000 ft^/s "source SALINITY 32 PPT. Figure 3-38. 200 190 180 170 160 100-FT CHANNEL STATIONS SHOALING DISTRIBUTION Verification of shoaling distribution, Umpqua River Estuary model (after Fisackerly, 1970). 115. Please note that these images are extracted from scanned page images that may ha

. The Biological bulletin. Biology; Zoology; Biology; Marine Biology. GENETICS OE MYTILUS 315 200- O z LJ LJ I LO 150- 100- SALINITY (%o) 30 16 11 x x. 5 10 15 DAYS FROM FERTILIZATION 20 EitiURK 2. Increase in mean length uf larvae raised at three salinities after development until day 3 at 30',',. Vertical bars indicate the least significant difference between means for each day ( cc =0.05). effects and salinity as a fixed effect. In the single-pair experiment, random families and fixed salinities were used as main effects in a two-way mixed model design. RESULTS 1C i '/JIT/ 0} salhii/v In th Stock Photo

RMRHN602–. The Biological bulletin. Biology; Zoology; Biology; Marine Biology. GENETICS OE MYTILUS 315 200- O z LJ LJ I LO 150- 100- SALINITY (%o) 30 16 11 x x. 5 10 15 DAYS FROM FERTILIZATION 20 EitiURK 2. Increase in mean length uf larvae raised at three salinities after development until day 3 at 30',',. Vertical bars indicate the least significant difference between means for each day ( cc =0.05). effects and salinity as a fixed effect. In the single-pair experiment, random families and fixed salinities were used as main effects in a two-way mixed model design. RESULTS 1C i '/JIT/ 0} salhii/v In th

. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 40W 30W ?0W I0W 0 »- ffOHU? 0,i.; MO^ TIC RUN COMtan IMTTBV*. • e lfW-83 fifio HIM SCALC FUCIOR ? 1WE-05 FIELD "»» «600.0 5000.0 • 344€-BI 118 5W 8*7 5HI ».37eE-»i 135.5»w. 02.911 4crw LONGITUOE 20* 0" IO*E. r 5000 m Figure 3.46 Zonal cross-section near 16°S latitude in the Atlantic Ocean of (a) salinity in units of 0.1 PPT for experiment 1 and (b) observed salinity in PPT (from Pickard and Emery, 1982). 90.. Please note that these images are extracted from scanned page images that may have bee Stock Photo

RMRNAJHJ–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 40W 30W ?0W I0W 0 »- ffOHU? 0,i.; MO^ TIC RUN COMtan IMTTBV*. • e lfW-83 fifio HIM SCALC FUCIOR ? 1WE-05 FIELD "»» «600.0 5000.0 • 344€-BI 118 5W 8*7 5HI ».37eE-»i 135.5»w. 02.911 4crw LONGITUOE 20* 0" IO*E. r 5000 m Figure 3.46 Zonal cross-section near 16°S latitude in the Atlantic Ocean of (a) salinity in units of 0.1 PPT for experiment 1 and (b) observed salinity in PPT (from Pickard and Emery, 1982). 90.. Please note that these images are extracted from scanned page images that may have bee

RMRCW809–. Development of a microcomputer coupled Atmospheric and Oceanic Boundary Layer prediction model.. Meteorology; Oceanography. Retreat Mode Compute Updated: Mixed layer depth Well mixed temperature (SST) Well mixed salinity. 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.. Tarbet, Gary Lee.. Monterey, California: U. S. Naval Postgraduate School

RMRCW80R–. Development of a microcomputer coupled Atmospheric and Oceanic Boundary Layer prediction model.. Meteorology; Oceanography. Prescribed Inputs: Surface wind speed and direction Incident Radiation Precipitation - Evaporation Surface (lm) Radiation Absorption Critical Richardson Number N/ Required Profiles: Temperature Salinity Velocity Compute: Surface Fluxes Stability Parameters. 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 wo

RMRCW803–. Development of a microcomputer coupled Atmospheric and Oceanic Boundary Layer prediction model.. Meteorology; Oceanography. Retreat Mode Compute Updated: Mixed layer depth Well mixed temperature (SST) Well mixed salinity. Figure 5. Input and Flow Chart for CBL Prediction Model 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.. Tarbet, Gary Lee.. Monterey, California: U. S. Naval Postgraduate School

Salinity model Stock Photos and Images

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