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| griddap | Subset | tabledap | Make A Graph | wms | files | Title | Summary | FGDC | ISO 19115 | Info | Background Info | RSS | Institution | Dataset ID | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| https://pallter-data.marine.rutgers.edu/erddap/tabledap/BirdCensusStationaryWinter.subset | https://pallter-data.marine.rutgers.edu/erddap/tabledap/BirdCensusStationaryWinter | https://pallter-data.marine.rutgers.edu/erddap/tabledap/BirdCensusStationaryWinter.graph | https://pallter-data.marine.rutgers.edu/erddap/files/BirdCensusStationaryWinter/ | At-sea seabird censuses. Data on the species encountered (including marine mammals), their abundance, distribution and behavior. Data collected aboard cruises off the coast of the Western Antarctic Penninsula, 1993, 1999 and 2001. | The objectives of the LTER seabird component during the 92-93 season cruises were similar. These objectives included 1) determining the pelagic abundance and distribution of Adelie Penguins, 2) examining how the physical and biological characteristics of the marine environment influence these parameters and, 3) using these data to identify foraging areas that may be important to Adelie populations being studied as part of land-based work at Palmer Station. Secondary objectives included documenting the abundance and distribution of other seabirds and marine mammals within the LTER study area. The focus of the January cruise was the nearshore foraging habitat,which required sampling at smaller scales. All seabird censuses were thus conducted within approximately 100 kms of Palmer Station while traversing a sampling grid with stations at 10km intervals. The first two days (18-20 January) of this cruise were spent covering the selected grid as rapidly as possible resulting in 45 transects spaced at 45-60 minute intervals. There were no stops at the 10km stations during this Fast Grid phase. Upon completion of the Fast Grid, a force 12 gale suspended data collection for 24 hours. From January 22-25 the grid direction was reversed and the grid repeated. During this Slow Grid phase, 2-M net tows were done at 10km intervals and BOPS and 1-M and 2-M net tows every 20 km. All seabird censusesduring the cruise were done using the procedures outlined in theprevious paragraph.\n\ncdm_data_type = Trajectory\nVARIABLES:\nevent\ncruise_id\nstudy_name (Study)\ndepth (m)\nlatitude (degrees_north)\nlongitude (degrees_east)\ntime (seconds since 1970-01-01T00:00:00Z)\nstation\ngrid_line (km)\ngrid_station (km)\nsea_state\nsalinity (Sea Water Practical Salinity, 1)\n... (14 more variables)\n | https://pallter-data.marine.rutgers.edu/erddap/metadata/fgdc/xml/BirdCensusStationaryWinter_fgdc.xml | https://pallter-data.marine.rutgers.edu/erddap/metadata/iso19115/xml/BirdCensusStationaryWinter_iso19115.xml | https://pallter-data.marine.rutgers.edu/erddap/info/BirdCensusStationaryWinter/index.htmlTable | https://pal.lternet.edu/
| http://pallter-data.marine.rutgers.edu/erddap/rss/BirdCensusStationaryWinter.rss | https://pallter-data.marine.rutgers.edu/erddap/subscriptions/add.html?datasetID=BirdCensusStationaryWinter&showErrors=false&email= | National Science Foundation | BirdCensusStationaryWinter | ||
| https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruiseDissolvedOxygen.subset | https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruiseDissolvedOxygen | https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruiseDissolvedOxygen.graph | https://pallter-data.marine.rutgers.edu/erddap/files/CruiseDissolvedOxygen/ | Dissolved oxygen of discrete water column samples at selected depths collected aboard Palmer LTER annual cruises off the coast of the Western Antarctic Peninsula, 1993, 2012. | Dissolved oxygen of discrete water column samples at selected depths collected aboard Palmer LTER annual cruises off the coast of the Western Antarctic Peninsula, 1993 - 2012. Oxygen is produced by phytoplankton photosynthesis and consumed by respiration of phytoplankton, zooplankton and bacteria. Oxygen also enters and exits the ocean via physical exchange with the atmosphere. Oxygen concentrations in the surface ocean may be supersaturated by photosynthesis and turbulence enhancing air-sea exchange via bubble injection; or undersaturated due to excess respiration. In cases where exchange with the atmosphere is limited, and/or respiration exceeds photosynthesis, oxygen concentration can be reduced to very low levels (hypoxia) or entirely depleted (anoxia). This is uncommon in cold Antarctic Seas where respiration is depressed and oxygen solubility is enhanced by low temperature. Different water masses have characteristic oxygen concentrations which serve as tracers for diagnosing physical mixing and advection. Dissolved oxygen was analyzed by Winkler Titration (see Methods) in Conductivity, Temperature, Depth (CTD)-Rosette bottle samples at all depths sampled until 2012. This measurement was discontinued in 2013. The CTD has duplicate oxygen electrodes that provide continuous vertical profiles of oxygen concentration at all depths on all casts. The vessel also has continuous underway, Optode determination of dissolved oxygen in the surface (ship's intake at 6 meters depth) on all cruises. Finally we now routinely measure net community production by Equilibrator Inlet Mass Spectroscopy (EIMS) on LTER cruises\n\ncdm_data_type = Trajectory\nVARIABLES:\nstudy_name (Study)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\nevent\ngrid_line\ngrid_station\nbottle\noxygen_concentration (mL L-1)\noxygen_concentration_moles (micromoles L-1)\ncomments\n | https://pallter-data.marine.rutgers.edu/erddap/metadata/fgdc/xml/CruiseDissolvedOxygen_fgdc.xml | https://pallter-data.marine.rutgers.edu/erddap/metadata/iso19115/xml/CruiseDissolvedOxygen_iso19115.xml | https://pallter-data.marine.rutgers.edu/erddap/info/CruiseDissolvedOxygen/index.htmlTable | https://pal.lternet.edu/
| http://pallter-data.marine.rutgers.edu/erddap/rss/CruiseDissolvedOxygen.rss | https://pallter-data.marine.rutgers.edu/erddap/subscriptions/add.html?datasetID=CruiseDissolvedOxygen&showErrors=false&email= | National Science Foundation | CruiseDissolvedOxygen | ||
| https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruiseInherentOpticalProperties.subset | https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruiseInherentOpticalProperties | https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruiseInherentOpticalProperties.graph | https://pallter-data.marine.rutgers.edu/erddap/files/CruiseInherentOpticalProperties/ | Inherent optical properties measured at selected water-column depths, collected aboard Palmer LTER Annual cruises off the coast of the Western Antarctic Penninsula, 2009. | The Palmer, Antarctica, Long-Term Ecological Research project is a member site of the Long-Term Ecological Research program, a network of sites investigating diverse biomes. A team of researchers seeks to understand the structure and function of the Western Antarctic Peninsula's marine and terrestrial ecosystems in the context of seasonal-to-interannual atmospheric and sea ice dynamics, as well as long-term climate change. The PAL measurement system (or grid) is designed to study marine and terrestrial food webs consisting principally of diatom primary producers, the dominant herbivore Antarctic krill, and the apex predator Adelie penguin. An attenuated microbial food web is also a focus. PAL studies these ecosystems annually over a regional scale grid of oceanographic stations and seasonally at Palmer Station. \\n\\nPalmer Station is located on Anvers Island west of the Antarctic Peninula. The peninsula runs perpendicular to a strong climatic gradient between the cold, dry continental regime to the south, characteristic of the Antarctic interior, and the warm, moist, maritime regime to the north. North-south shifts in the gradient give rise to large environmental variability to climate change. Sea ice extent and variability affects ecosystem changes at all trophic levels. In addition to the long-term field and research activities, information management, graduate student training, education and outreach are an integral part of the program.\n\ncdm_data_type = Trajectory\nVARIABLES:\nstudy_name (Study)\nevent\ntime (seconds since 1970-01-01T00:00:00Z)\ngrid_line\ngrid_station\nstation\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\nsalinity (Sea Water Practical Salinity, 1)\ntemperature (Sea Water Temperature, degree_C)\nconductivity (Sea Water Electrical Conductivity, mS cm-1)\n... (24 more variables)\n | https://pallter-data.marine.rutgers.edu/erddap/metadata/fgdc/xml/CruiseInherentOpticalProperties_fgdc.xml | https://pallter-data.marine.rutgers.edu/erddap/metadata/iso19115/xml/CruiseInherentOpticalProperties_iso19115.xml | https://pallter-data.marine.rutgers.edu/erddap/info/CruiseInherentOpticalProperties/index.htmlTable | https://pal.lternet.edu/
| http://pallter-data.marine.rutgers.edu/erddap/rss/CruiseInherentOpticalProperties.rss | https://pallter-data.marine.rutgers.edu/erddap/subscriptions/add.html?datasetID=CruiseInherentOpticalProperties&showErrors=false&email= | National Science Foundation | CruiseInherentOpticalProperties | ||
| https://pallter-data.marine.rutgers.edu/erddap/tabledap/StandardBodyLengthsSalpathompsoni.subset | https://pallter-data.marine.rutgers.edu/erddap/tabledap/StandardBodyLengthsSalpathompsoni | https://pallter-data.marine.rutgers.edu/erddap/tabledap/StandardBodyLengthsSalpathompsoni.graph | https://pallter-data.marine.rutgers.edu/erddap/files/StandardBodyLengthsSalpathompsoni/ | Length of Salpa thompsoni collected with a 2-m, 700-um net towed from surface to 120 m, collected aboard Palmer LTER annual cruises off the coast of the Western Antarctic Peninsula, 2009, 2019. | Length of Salpa thompsoni collected with a 2-m, 700-um net towed from surface to 120 m, collected aboard Palmer LTER annual cruises off the coast of the Western Antarctic Peninsula, 2009 - 2019. Salps (Salpa thompsoni) are conspicuous gelatinous zooplankton capable of rapid population increases, enabling them to respond quickly to unpredictable phytoplankton blooms common in the Antarctic. Body length was measured on salps collected from LTER zooplankton tows along the western Antarctic Peninsula. Salps have amongst the highest filtration rates of all zooplankton, and package their waste into large, fast sinking fecal pellets. These pellets provide a mechanism to export carbon fixed in the surface waters into the deep ocean. Since filtration rates and pellet size are positively related to the size of a salp, population estimates of grazing and exported carbon can be determined through length data.\\n\n\ncdm_data_type = Trajectory\nVARIABLES:\ncruise_tow_number\ncruise_name\nevent\ntow_number\ngrid_line\ngrid_station\ntime (Start Time, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\nend_time (seconds since 1970-01-01T00:00:00Z)\nlat_end (Latitude, degrees_north)\nlon_end (Longitude, degrees_east)\ntow_duration (minutes)\nheading (degrees)\nspeed_over_ground\ndepth (m)\nwind_speed (m s-1)\nwind_direction (Wind To Direction, degrees)\n... (7 more variables)\n | https://pallter-data.marine.rutgers.edu/erddap/metadata/fgdc/xml/StandardBodyLengthsSalpathompsoni_fgdc.xml | https://pallter-data.marine.rutgers.edu/erddap/metadata/iso19115/xml/StandardBodyLengthsSalpathompsoni_iso19115.xml | https://pallter-data.marine.rutgers.edu/erddap/info/StandardBodyLengthsSalpathompsoni/index.htmlTable | https://pal.lternet.edu/
| http://pallter-data.marine.rutgers.edu/erddap/rss/StandardBodyLengthsSalpathompsoni.rss | https://pallter-data.marine.rutgers.edu/erddap/subscriptions/add.html?datasetID=StandardBodyLengthsSalpathompsoni&showErrors=false&email= | National Science Foundation | StandardBodyLengthsSalpathompsoni | ||
| https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruiseEventLog.subset | https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruiseEventLog | https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruiseEventLog.graph | https://pallter-data.marine.rutgers.edu/erddap/files/CruiseEventLog/ | Palmer (PAL) log of events aboard Palmer LTER cruises off the coast of the Western Antarctic Peninsula (cruise happenings ordered by time) is a meta dataset, including lat-lon, datetime, activity, events, etc, 1991, 2019. | Palmer (PAL) log of events aboard Palmer LTER cruises off the coast of the Western Antarctic Peninsula (cruise happenings ordered by time) is a meta dataset, including lat-lon, datetime, activity, events, etc, 1991 - 2019. The event log for the Palmer LTER research cruises provides a mapping of sampling and other research activities to spatial, temporal and other variables. Event numbers are used to coordinate relational indexes and provide users of the data with a high-level index for relating measurements across research components.\n\ncdm_data_type = Trajectory\nVARIABLES:\nstudy_name (Study)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\nevent\nevent_group\ncast_number\nevent_name\ngrid_station\nstation\ngrid_line\ncalculated_grid_station\ncomments\nnotes\n | https://pallter-data.marine.rutgers.edu/erddap/metadata/fgdc/xml/CruiseEventLog_fgdc.xml | https://pallter-data.marine.rutgers.edu/erddap/metadata/iso19115/xml/CruiseEventLog_iso19115.xml | https://pallter-data.marine.rutgers.edu/erddap/info/CruiseEventLog/index.htmlTable | https://pal.lternet.edu/
| http://pallter-data.marine.rutgers.edu/erddap/rss/CruiseEventLog.rss | https://pallter-data.marine.rutgers.edu/erddap/subscriptions/add.html?datasetID=CruiseEventLog&showErrors=false&email= | National Science Foundation | CruiseEventLog | ||
| https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruisePhotosyntheticParametersfromPhotosynthesisIrradianceCurves.subset | https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruisePhotosyntheticParametersfromPhotosynthesisIrradianceCurves | https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruisePhotosyntheticParametersfromPhotosynthesisIrradianceCurves.graph | https://pallter-data.marine.rutgers.edu/erddap/files/CruisePhotosyntheticParametersfromPhotosynthesisIrradianceCurves/ | Photosynthesis-irradiance measurements used to derive P-I relationships and to calculate primary production for each discrete sample. Samples collected aboard Palmer LTER annual cruises off the coast of the Western Antarctic Peninsula, 1991, 1993. | Photosynthesis-irradiance measurements used to derive P-I relationships and to calculate primary production for each discrete sample. Samples collected aboard Palmer LTER annual cruises off the coast of the Western Antarctic Peninsula, 1991 - 1993. Photosynthesis-irradiance measurements are used to derive P-I relationships and to calculate primary production for each discrete sample. Blue-green photosynthetron method described by Prezelin et al. (1994) were used to determine photosynthesis irradiance (P-I) relationships for collected samples. Non-linear cureve fits for the P-I data were calculated using the simplex method of Caceci & Cacheris (1984). Curve fitting provided estimates of Pmax (the light saturated rate of photosynthesis) and alpha (the affinity for photosynthesis at light-limited irradiances.\n\ncdm_data_type = Trajectory\nVARIABLES:\nstudy_name (Study)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\nevent (Event Number)\njulian_day\nincubation_start_time (seconds since 1970-01-01T00:00:00Z)\ngrid_station\nstation\ngrid_line\nbottle (Bottle Number)\ndepth (m)\nchlorophyll_a (mg m-3)\nincubation_hours (Incubation Hrs, hours)\nin_situ_temperature (In Situ Water Temperature, degree_C)\nincubation_temperature (Incubation Water Temperature, degree_C)\npmax (mg m-3 hour-1)\nalpha\nbeta (percent)\n... (8 more variables)\n | https://pallter-data.marine.rutgers.edu/erddap/metadata/fgdc/xml/CruisePhotosyntheticParametersfromPhotosynthesisIrradianceCurves_fgdc.xml | https://pallter-data.marine.rutgers.edu/erddap/metadata/iso19115/xml/CruisePhotosyntheticParametersfromPhotosynthesisIrradianceCurves_iso19115.xml | https://pallter-data.marine.rutgers.edu/erddap/info/CruisePhotosyntheticParametersfromPhotosynthesisIrradianceCurves/index.htmlTable | https://pal.lternet.edu/
| http://pallter-data.marine.rutgers.edu/erddap/rss/CruisePhotosyntheticParametersfromPhotosynthesisIrradianceCurves.rss | https://pallter-data.marine.rutgers.edu/erddap/subscriptions/add.html?datasetID=CruisePhotosyntheticParametersfromPhotosynthesisIrradianceCurves&showErrors=false&email= | National Science Foundation | CruisePhotosyntheticParametersfromPhotosynthesisIrradianceCurves | ||
| https://pallter-data.marine.rutgers.edu/erddap/tabledap/StandardBodyLengthsESuperba.subset | https://pallter-data.marine.rutgers.edu/erddap/tabledap/StandardBodyLengthsESuperba | https://pallter-data.marine.rutgers.edu/erddap/tabledap/StandardBodyLengthsESuperba.graph | https://pallter-data.marine.rutgers.edu/erddap/files/StandardBodyLengthsESuperba/ | Standard body length of Euphausia superba collected with a 2-m, 700-um net towed from surface to 120 m, collected aboard Palmer LTER annual cruises off the coast of the Western Antarctic Peninsula, 2009, 2019. | Standard body length of Euphausia superba collected with a 2-m, 700-um net towed from surface to 120 m, collected aboard Palmer LTER annual cruises off the coast of the Western Antarctic Peninsula, 2009 - 2019. Antarctic krill, Euphausia superba, are a critical food-web link between phytoplankton primary production and higher trophic levels, such as whales, penguins, and seals. Krill standard length was measured from LTER zooplankton tows along the western Antarctic Peninsula. Length data provides estimates of age-class abundance and recruitment. Climate-induced changes in krill recruitment are an important consideration in the management and modelling of krill populations.\\n\n\ncdm_data_type = Trajectory\nVARIABLES:\ncruise_tow_number\ncruise_name\nevent\ntow_number\ngrid_line\ngrid_station\ntime (Start Time, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\nend_time (seconds since 1970-01-01T00:00:00Z)\nlat_end (Latitude, degrees_north)\nlon_end (Longitude, degrees_east)\ntow_duration (minutes)\nheading (degrees)\nspeed_over_ground\ndepth (m)\nwind_speed (m s-1)\nwind_direction (Wind To Direction, degrees)\nnet_id\ntow_type\n... (5 more variables)\n | https://pallter-data.marine.rutgers.edu/erddap/metadata/fgdc/xml/StandardBodyLengthsESuperba_fgdc.xml | https://pallter-data.marine.rutgers.edu/erddap/metadata/iso19115/xml/StandardBodyLengthsESuperba_iso19115.xml | https://pallter-data.marine.rutgers.edu/erddap/info/StandardBodyLengthsESuperba/index.htmlTable | https://pal.lternet.edu/
| http://pallter-data.marine.rutgers.edu/erddap/rss/StandardBodyLengthsESuperba.rss | https://pallter-data.marine.rutgers.edu/erddap/subscriptions/add.html?datasetID=StandardBodyLengthsESuperba&showErrors=false&email= | National Science Foundation | StandardBodyLengthsESuperba | ||
| https://pallter-data.marine.rutgers.edu/erddap/tabledap/ZooplanktonDensityHistorical.subset | https://pallter-data.marine.rutgers.edu/erddap/tabledap/ZooplanktonDensityHistorical | https://pallter-data.marine.rutgers.edu/erddap/tabledap/ZooplanktonDensityHistorical.graph | https://pallter-data.marine.rutgers.edu/erddap/files/ZooplanktonDensityHistorical/ | Zooplankton collected aboard Palmer Station LTER annual cruises off the western antarctic peninsula, 1993, 2008. | Zooplankton collected aboard Palmer Station LTER annual cruises off the western antarctic peninsula, 1993 - 2008. Samples were collected with a 2-m, 700-um net towed from surface to 120 m. This dataset is the historical (1993 - 2008) counterpart to dataset #199, Zooplankton Density - Current. Together these two data sets comprise the full Palmer LTER zooplankton density time series. Please refer to the methods of each dataset for differences between the two.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntime (Start Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nlatitude (degrees_north)\nlongitude (degrees_east)\nend_time (seconds since 1970-01-01T00:00:00Z)\nlat_end (Latitude, degrees_north)\nlon_end (Longitude, degrees_east)\ncruise_tow_number\ncruise_name\nevent\ntow_number\ngrid_line\ngrid_station\ntow_duration (minutes)\nheading (degrees)\nspeed_over_ground\nwind_speed_start (Wind Speed)\nwind_direction (Wind From Direction, degrees)\nnet_id\ntow_type\ntarget_depth (Depth)\ndepth_max (Depth, meters)\nvolume_filtered (m3)\n... (60 more variables)\n | https://pallter-data.marine.rutgers.edu/erddap/metadata/fgdc/xml/ZooplanktonDensityHistorical_fgdc.xml | https://pallter-data.marine.rutgers.edu/erddap/metadata/iso19115/xml/ZooplanktonDensityHistorical_iso19115.xml | https://pallter-data.marine.rutgers.edu/erddap/info/ZooplanktonDensityHistorical/index.htmlTable | https://pal.lternet.edu/
| http://pallter-data.marine.rutgers.edu/erddap/rss/ZooplanktonDensityHistorical.rss | https://pallter-data.marine.rutgers.edu/erddap/subscriptions/add.html?datasetID=ZooplanktonDensityHistorical&showErrors=false&email= | National Science Foundation | ZooplanktonDensityHistorical | ||
| https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruiseZooplanktonAbundance.subset | https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruiseZooplanktonAbundance | https://pallter-data.marine.rutgers.edu/erddap/tabledap/CruiseZooplanktonAbundance.graph | https://pallter-data.marine.rutgers.edu/erddap/files/CruiseZooplanktonAbundance/ | Zooplankton collected with a 1.4 m2 frame, 500-µm mesh Multiple Opening/Closing Net and Environmental Sensing System (MOCNESS) aboard Palmer LTER annual cruises off the coast of the Western Antarctic Peninsula, 2009-2017 | Zooplankton are a morphologically and taxonomically diverse group of animals. Many zooplankton feed on phytoplankton in surface waters and thus provide a link between primary producers and higher trophic levels. Other zooplankton reside in the mesopelagic zone and feed on detritus or on other animals. Depth-discrete density of zooplankton taxa was determined at process study stations on the annual Palmer LTER cruises along the western Antarctic Peninsula. Samples were collected with a 1.4-m2 frame, 500-μm mesh Multiple Opening/Closing Net and Environmental Sensing System (MOCNESS) towed obliquely to the surface from a depth of typically 500 m. MOCNESS tows were conducted in consecutive day-night pairs at each process study station. Zooplankton depth distributions vary between day and night as these animals conduct diel vertical migrations. Depth distributions also vary among zooplankton taxa based on species feeding ecology and life history traits. Zooplankton diel vertical migration contributes to the export of carbon and nutrients from the surface ocean to the mesopelagic zone.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntow_start_datetime (MOCNESS start datetime, seconds since 1970-01-01T00:00:00Z)\ntow_end_datetime (MOCNESS end datetime, seconds since 1970-01-01T00:00:00Z)\nlatitude (Net Lat Avg, degrees_north)\nlongitude (Net Lon Avg, degrees_east)\ncruise_name\ngrid_line\ngrid_station\namphipoda\ncacutus\nchaetognatha\ncpropinquus\necrystal\ngymnosomata\nlhelicina\nmgerlachei\nostracoda\n... (28 more variables)\n | https://pallter-data.marine.rutgers.edu/erddap/metadata/fgdc/xml/CruiseZooplanktonAbundance_fgdc.xml | https://pallter-data.marine.rutgers.edu/erddap/info/CruiseZooplanktonAbundance/index.htmlTable | https://pal.lternet.edu/
| http://pallter-data.marine.rutgers.edu/erddap/rss/CruiseZooplanktonAbundance.rss | https://pallter-data.marine.rutgers.edu/erddap/subscriptions/add.html?datasetID=CruiseZooplanktonAbundance&showErrors=false&email= | Rutgers University | CruiseZooplanktonAbundance | |||
| https://pallter-data.marine.rutgers.edu/erddap/tabledap/ZooplanktonDensityCurrent.subset | https://pallter-data.marine.rutgers.edu/erddap/tabledap/ZooplanktonDensityCurrent | https://pallter-data.marine.rutgers.edu/erddap/tabledap/ZooplanktonDensityCurrent.graph | https://pallter-data.marine.rutgers.edu/erddap/files/ZooplanktonDensityCurrent/ | Zooplankton collected with a 2-m, 700-um net towed from surface to 120 m, aboard Palmer Station Antarctica LTER annual cruises off the western antarctic peninsula, 2009, 2019. | Zooplankton collected with a 2-m, 700-um net towed from surface to 120 m, aboard Palmer Station Antarctica LTER annual cruises off the western antarctic peninsula, 2009 - 2019. Zooplankton are a morphologically and taxonomically diverse group of animals. Many zooplankton feed on phytoplankton and thus provide a link between primary producers and higher trophic levels. Zooplankton density and biovolume were determined at grid stations on the annual LTER cruises along the western Antarctic Peninsula (WAP). Typically, zooplankton were collected with a 2x2 meter, 700um mesh net fitted with a flow meter and towed obliquely to 120m. Zooplankton distributions vary spatially due to water column characteristics, which affect their predators' distributions. As climate change continues to affect the WAP, the relative abundance of the various zooplankton components can also be expected to change.\\n\\n\n\ncdm_data_type = Trajectory\nVARIABLES:\ntime (Start Time, seconds since 1970-01-01T00:00:00Z)\nend_time (seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nlatitude (degrees_north)\nlongitude (degrees_east)\nlat_end (Latitude, degrees_north)\nlon_end (Longitude, degrees_east)\ncruise_name\nevent\ncruise_tow_number\ngrid_line\ngrid_station\ntow_duration\nheading (degrees)\nspeed_over_ground\nwind_speed_start (Wind Speed, m s-1)\nnet_id\ntow_type\n... (90 more variables)\n | https://pallter-data.marine.rutgers.edu/erddap/metadata/fgdc/xml/ZooplanktonDensityCurrent_fgdc.xml | https://pallter-data.marine.rutgers.edu/erddap/metadata/iso19115/xml/ZooplanktonDensityCurrent_iso19115.xml | https://pallter-data.marine.rutgers.edu/erddap/info/ZooplanktonDensityCurrent/index.htmlTable | https://pal.lternet.edu/
| http://pallter-data.marine.rutgers.edu/erddap/rss/ZooplanktonDensityCurrent.rss | https://pallter-data.marine.rutgers.edu/erddap/subscriptions/add.html?datasetID=ZooplanktonDensityCurrent&showErrors=false&email= | National Science Foundation | ZooplanktonDensityCurrent |