![]() |
ERDDAP
Easier access to scientific data |
Brought to you by NOAA NMFS SWFSC ERD |
Grid DAP Data | Sub- set | Table DAP Data | Make A Graph | W M S | Source Data Files | Title | Sum- mary | FGDC, ISO, Metadata | Back- ground Info | RSS | E | Institution | Dataset ID | ||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
set | data | graph | files | Vertical fluxes of particulate carbon, nitrogen and phosphorus from a sediment trap deployed west of Palmer Station, Antarctica at a depth of 170 meters, 1992-present. | ![]() | M | background![]() | ![]() | ![]() |
| OffshoreSedimentTrapFluxes |
Row Type | Variable Name | Attribute Name | Data Type | Value |
---|---|---|---|---|
attribute | NC_GLOBAL | _NCProperties | String | version=1|netcdflibversion=4.6.1|hdf5libversion=1.10.6 |
attribute | NC_GLOBAL | acknowledgement | String | Funding and support provided by the National Science Foundation |
attribute | NC_GLOBAL | cdm_data_type | String | Other |
attribute | NC_GLOBAL | comment | String | 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. |
attribute | NC_GLOBAL | contributor_email | String | hducklow@ldeo.columbia.edu,sharon.stammerjohn@colorado.edu,dkarl@hawaii.edu,chriscarri@yahoo.com |
attribute | NC_GLOBAL | contributor_name | String | Hugh Ducklow,Sharon Stammerjohn,David Karl,Christopher Carrillo |
attribute | NC_GLOBAL | contributor_role | String | PrincipalInvestigator,PrincipalInvestigator,PrincipalInvestigator,PrincipalInvestigator |
attribute | NC_GLOBAL | contributor_role_vocabulary | String | https://vocab.nerc.ac.uk/collection/G04/current/![]() |
attribute | NC_GLOBAL | Conventions | String | CF-1.8, ACDD-1.3, COARDS |
attribute | NC_GLOBAL | creator_country | String | USA |
attribute | NC_GLOBAL | creator_email | String | kerfoot at marine.rutgers.edu |
attribute | NC_GLOBAL | creator_institution | String | Rutgers University |
attribute | NC_GLOBAL | creator_name | String | John Kerfoot |
attribute | NC_GLOBAL | creator_sector | String | academic |
attribute | NC_GLOBAL | creator_type | String | person |
attribute | NC_GLOBAL | creator_url | String | https://rucool.marine.rutgers.edu![]() |
attribute | NC_GLOBAL | datazoo_dataset_id | String | 26 |
attribute | NC_GLOBAL | datazoo_datatable_id | String | 26 |
attribute | NC_GLOBAL | datazoo_datatable_label | String | Offshore Sediment Trap Fluxes |
attribute | NC_GLOBAL | datazoo_datatable_name | String | OffshoreSedimentTrapFluxes |
attribute | NC_GLOBAL | date_created | String | 2021-08-04T18:17:56Z |
attribute | NC_GLOBAL | date_issued | String | 2021-08-04T18:17:56Z |
attribute | NC_GLOBAL | defaultDataQuery | String | null |
attribute | NC_GLOBAL | defaultGraphQuery | String | time,carbon_flux&.draw=markers&.marker=6%7C5&.color=0x000000&.colorBar=%7C%7C%7C%7C%7C&.bgColor=0xffccccff&.yRange=0%7C%7Ctrue%7C |
attribute | NC_GLOBAL | doi | String | https://doi.org/10.6073/pasta/c0a2d3a87876ff3baddad20343b6483d![]() |
attribute | NC_GLOBAL | geospatial_bounds_crs | String | EPSG:4326 |
attribute | NC_GLOBAL | geospatial_bounds_vertical_crs | String | EPSG:5831 |
attribute | NC_GLOBAL | geospatial_lat_resolution | String | 0.00001 degree |
attribute | NC_GLOBAL | geospatial_lat_units | String | degree_north |
attribute | NC_GLOBAL | geospatial_lon_resolution | String | 0.00001 degree |
attribute | NC_GLOBAL | geospatial_lon_units | String | degree_east |
attribute | NC_GLOBAL | geospatial_vertical_positive | String | down |
attribute | NC_GLOBAL | geospatial_vertical_units | String | EPSG:5831 |
attribute | NC_GLOBAL | history | String | local files |
attribute | NC_GLOBAL | infoUrl | String | https://pal.lternet.edu/![]() |
attribute | NC_GLOBAL | institution | String | National Science Foundation |
attribute | NC_GLOBAL | keywords | String | carbon flux, nitrogen flux, Organic Matter, organic matter, particulate organic carbon, sediments, Signature |
attribute | NC_GLOBAL | keywords_vocabulary | String | LTER Controlled Vocabulary,LTER Core Areas |
attribute | NC_GLOBAL | license | String | All data contained herein is licensed under the LTER Network Data Access Policy (https://lternet.edu/data-access-policy/)![]() |
attribute | NC_GLOBAL | license_link | String | https://lternet.edu/data-access-policy/![]() |
attribute | NC_GLOBAL | methods | String | Samping Methods: Palmer LTER deploys a McLane Mark IV PARFLUX 21H sediment trap. This is the same design and deployment protocol employed by the former US JGOFS Time Series sites at Bermuda in the Ocean Flux Program (http://ecosystems.mbl.edu/conte/ofp/)\t![]() |
attribute | NC_GLOBAL | naming_authority | String | edu.rutgers.rucool |
attribute | NC_GLOBAL | product_version | String | 1.0 |
attribute | NC_GLOBAL | program | String | LTER |
attribute | NC_GLOBAL | project | String | Palmer LTER |
attribute | NC_GLOBAL | publisher_country | String | USA |
attribute | NC_GLOBAL | publisher_email | String | kerfoot at marine.rutgers.edu |
attribute | NC_GLOBAL | publisher_institution | String | Rutgers University |
attribute | NC_GLOBAL | publisher_name | String | John Kerfoot |
attribute | NC_GLOBAL | publisher_type | String | person |
attribute | NC_GLOBAL | publisher_url | String | https://rucool.marine.rutgers.edu![]() |
attribute | NC_GLOBAL | references | String | https://pal.lternet.edu/![]() |
attribute | NC_GLOBAL | sea_name | String | Southern Ocean |
attribute | NC_GLOBAL | source | String | local files |
attribute | NC_GLOBAL | sourceUrl | String | (local files) |
attribute | NC_GLOBAL | standard_name_vocabulary | String | CF Standard Name Table v77 |
attribute | NC_GLOBAL | subsetVariables | String | study_name |
attribute | NC_GLOBAL | summary | String | Particulate organic matter is exported from the upper ocean euphotic zone in the form of large sinking particles and as dissolved material. Particle fluxes to depth link the surface and mesopelagic realm and supply food to the benthos. Sedimentation flux is typically measured with sediment traps of various designs. Palmer LTER has deployed a time-series trap near 64.5degrees S, 66.0degrees W since late 1992. The trap is moored in 300 m depth and collects sinking particles at 150 m. Deployments and analyses were performed by David Karl, University of Hawaii until 2002 when Hugh Ducklow took over the sediment trap operations.Sedimentation at the PAL site of the West Antarctic Peninsula demonstrates extreme seasonality, with a well-defined pulse in the Austral summer following sea ice retreat. Daily sedimentation rates during the summer flux event are among the highest recorded globally. During the Austral winter when the ocean is covered by sea ice and shrouded in darkness, fluxes are among the lowest observed anywhere. Sedimentation rates at PAL typically vary by 4 orders of magnitude. There is also order of magnitude variability in the total annual flux (area under the curve)..Particulate organic matter is exported from the upper ocean euphotic zone in the form of large sinking particles and as dissolved material. Particle fluxes to depth link the surface and mesopelagic realm and supply food to the benthos. Sedimentation flux is typically measured with sediment traps of various designs. Palmer LTER has deployed a time-series trap near 64.5degrees S, 66.0degrees W since late 1992. The trap is moored in 300 m depth and collects sinking particles at 150 m. Deployments and analyses were performed by David Karl, University of Hawaii until 2002 when Hugh Ducklow took over the sediment trap operations.Sedimentation at the PAL site of the West Antarctic Peninsula demonstrates extreme seasonality, with a well-defined pulse in the Austral summer following sea ice retreat. Daily sedimentation rates during the summer flux event are among the highest recorded globally. During the Austral winter when the ocean is covered by sea ice and shrouded in darkness, fluxes are among the lowest observed anywhere. Sedimentation rates at PAL typically vary by 4 orders of magnitude. There is also order of magnitude variability in the total annual flux (area under the curve)..Particulate organic matter is exported from the upper ocean euphotic zone in the form of large sinking particles and as dissolved material. Particle fluxes to depth link the surface and mesopelagic realm and supply food to the benthos. Sedimentation flux is typically measured with sediment traps of various designs. Palmer LTER has deployed a time-series trap near 64.5degrees S, 66.0degrees W since late 1992. The trap is moored in 300 m depth and collects sinking particles at 150 m. Deployments and analyses were performed by David Karl, University of Hawaii until 2002 when Hugh Ducklow took over the sediment trap operations.Sedimentation at the PAL site of the West Antarctic Peninsula demonstrates extreme seasonality, with a well-defined pulse in the Austral summer following sea ice retreat. Daily sedimentation rates during the summer flux event are among the highest recorded globally. During the Austral winter when the ocean is covered by sea ice and shrouded in darkness, fluxes are among the lowest observed anywhere. Sedimentation rates at PAL typically vary by 4 orders of magnitude. There is also order of magnitude variability in the total annual flux (area under the curve). |
attribute | NC_GLOBAL | time_coverage_end | String | 2013-01-27T00:00:00Z |
attribute | NC_GLOBAL | time_coverage_start | String | 1992-11-10T00:00:00Z |
attribute | NC_GLOBAL | title | String | Vertical fluxes of particulate carbon, nitrogen and phosphorus from a sediment trap deployed west of Palmer Station, Antarctica at a depth of 170 meters, 1992-present. |
variable | study_name | String | ||
attribute | study_name | column_name | String | studyName |
attribute | study_name | comment | String | Cruise name |
attribute | study_name | ioos_category | String | Identifier |
attribute | study_name | long_name | String | Study |
variable | record_number | short | ||
attribute | record_number | _FillValue | short | 32767 |
attribute | record_number | actual_range | short | 1, 427 |
attribute | record_number | colorBarMaximum | double | 100.0 |
attribute | record_number | colorBarMinimum | double | 0.0 |
attribute | record_number | column_id | long | 306 |
attribute | record_number | column_name | String | col_306 |
attribute | record_number | ioos_category | String | Statistics |
attribute | record_number | long_name | String | Record Number |
attribute | record_number | lter_column_description | String | record number of a sampling event |
attribute | record_number | lter_column_name | String | Record |
attribute | record_number | lter_mscale | String | interval |
attribute | record_number | lter_num_type | String | natural |
attribute | record_number | lter_units_string | String | number |
attribute | record_number | units_conventions | String | EML-2.0.1,EML-2.1.0,EML-LTER |
variable | deployment_number | short | ||
attribute | deployment_number | _FillValue | short | 32767 |
attribute | deployment_number | actual_range | short | 1, 21 |
attribute | deployment_number | colorBarMaximum | double | 100.0 |
attribute | deployment_number | colorBarMinimum | double | 0.0 |
attribute | deployment_number | column_id | long | 307 |
attribute | deployment_number | column_name | String | col_307 |
attribute | deployment_number | ioos_category | String | Statistics |
attribute | deployment_number | long_name | String | Deployment Number |
attribute | deployment_number | lter_column_description | String | deployment number |
attribute | deployment_number | lter_column_name | String | Deployment |
attribute | deployment_number | lter_mscale | String | interval |
attribute | deployment_number | lter_num_type | String | natural |
attribute | deployment_number | lter_units_string | String | number |
attribute | deployment_number | units_conventions | String | EML-2.0.1,EML-2.1.0,EML-LTER |
variable | time | double | ||
attribute | time | _CoordinateAxisType | String | Time |
attribute | time | actual_range | double | 7.213536E8, 1.3592448E9 |
attribute | time | axis | String | T |
attribute | time | calendar | String | proleptic_gregorian |
attribute | time | column_id | long | 313 |
attribute | time | column_name | String | col_313 |
attribute | time | ioos_category | String | Time |
attribute | time | long_name | String | Time |
attribute | time | lter_column_description | String | date in GMT |
attribute | time | lter_column_name | String | Mid-date |
attribute | time | lter_mscale | String | dateTime |
attribute | time | standard_name | String | time |
attribute | time | time_origin | String | 01-JAN-1970 00:00:00 |
attribute | time | units | String | seconds since 1970-01-01T00:00:00Z |
variable | start_date | double | ||
attribute | start_date | actual_range | double | 7.210944E8, 1.3589856E9 |
attribute | start_date | calendar | String | proleptic_gregorian |
attribute | start_date | column_id | long | 310 |
attribute | start_date | column_name | String | col_310 |
attribute | start_date | ioos_category | String | Time |
attribute | start_date | long_name | String | Start Date |
attribute | start_date | lter_column_description | String | date in GMT |
attribute | start_date | lter_column_name | String | Start Date |
attribute | start_date | lter_mscale | String | dateTime |
attribute | start_date | standard_name | String | time |
attribute | start_date | time_origin | String | 01-JAN-1970 00:00:00 |
attribute | start_date | units | String | seconds since 1970-01-01T00:00:00Z |
variable | end_date | double | ||
attribute | end_date | actual_range | double | 7.216992E8, 1.3595904E9 |
attribute | end_date | calendar | String | proleptic_gregorian |
attribute | end_date | column_id | long | 311 |
attribute | end_date | column_name | String | col_311 |
attribute | end_date | ioos_category | String | Time |
attribute | end_date | long_name | String | End Date |
attribute | end_date | lter_column_description | String | date in GMT |
attribute | end_date | lter_column_name | String | End Date |
attribute | end_date | lter_mscale | String | dateTime |
attribute | end_date | standard_name | String | time |
attribute | end_date | time_origin | String | 01-JAN-1970 00:00:00 |
attribute | end_date | units | String | seconds since 1970-01-01T00:00:00Z |
variable | trap_id | byte | ||
attribute | trap_id | _FillValue | byte | 127 |
attribute | trap_id | actual_range | byte | 1, 4 |
attribute | trap_id | column_id | long | 308 |
attribute | trap_id | column_name | String | col_308 |
attribute | trap_id | ioos_category | String | Identifier |
attribute | trap_id | long_name | String | Trap Id |
attribute | trap_id | lter_column_description | String | identification number of sediment trap cup |
attribute | trap_id | lter_column_name | String | Trap |
attribute | trap_id | lter_mscale | String | interval |
attribute | trap_id | lter_num_type | String | integer |
attribute | trap_id | lter_units_string | String | number |
attribute | trap_id | units_conventions | String | EML-2.0.1,EML-2.1.0,EML-LTER |
variable | cup_number | byte | ||
attribute | cup_number | _FillValue | byte | 127 |
attribute | cup_number | actual_range | byte | 1, 21 |
attribute | cup_number | colorBarMaximum | double | 100.0 |
attribute | cup_number | colorBarMinimum | double | 0.0 |
attribute | cup_number | column_id | long | 309 |
attribute | cup_number | column_name | String | col_309 |
attribute | cup_number | ioos_category | String | Statistics |
attribute | cup_number | long_name | String | Cup Number |
attribute | cup_number | lter_column_description | String | identification number of sediment trap cup |
attribute | cup_number | lter_column_name | String | Cup |
attribute | cup_number | lter_mscale | String | interval |
attribute | cup_number | lter_num_type | String | natural |
attribute | cup_number | lter_units_string | String | number |
attribute | cup_number | units_conventions | String | EML-2.0.1,EML-2.1.0,EML-LTER |
variable | duration | double | ||
attribute | duration | _FillValue | double | 9.969209968386869E36 |
attribute | duration | actual_range | double | 4.0, 92.0 |
attribute | duration | column_id | long | 312 |
attribute | duration | column_name | String | col_312 |
attribute | duration | ioos_category | String | Unknown |
attribute | duration | long_name | String | Duration |
attribute | duration | lter_column_description | String | measure of the passing of time |
attribute | duration | lter_column_name | String | Duration |
attribute | duration | lter_mscale | String | ratio |
attribute | duration | lter_num_type | String | natural |
attribute | duration | lter_units_string | String | nominalDay |
attribute | duration | units_conventions | String | AND-LTER,EML-2.0.1,EML-2.1.0,EML-LTER,SGS-LTER |
variable | carbon_flux | double | ||
attribute | carbon_flux | _FillValue | double | 9.969209968386869E36 |
attribute | carbon_flux | actual_range | double | -9998.0, 123.69 |
attribute | carbon_flux | column_id | long | 314 |
attribute | carbon_flux | column_name | String | col_314 |
attribute | carbon_flux | ioos_category | String | CO2 |
attribute | carbon_flux | long_name | String | Carbon Flux |
attribute | carbon_flux | lter_column_description | String | a non-metallic element in the Periodic Table with Atomic Number 6, Atomic Weight 12.0107 |
attribute | carbon_flux | lter_column_name | String | Carbon Flux |
attribute | carbon_flux | lter_mscale | String | ratio |
attribute | carbon_flux | lter_num_type | String | real |
attribute | carbon_flux | lter_units | String | mg/m²/day |
attribute | carbon_flux | lter_units_string | String | milligramPerMeterSquaredPerDay |
attribute | carbon_flux | units | String | mg m-2 day-1 |
attribute | carbon_flux | units_conventions | String | HFR-LTER,PAL-LTER,SBC-LTER |
variable | nitrogen_flux | double | ||
attribute | nitrogen_flux | _FillValue | double | 9.969209968386869E36 |
attribute | nitrogen_flux | actual_range | double | -9998.0, 15.9 |
attribute | nitrogen_flux | column_id | long | 315 |
attribute | nitrogen_flux | column_name | String | col_315 |
attribute | nitrogen_flux | ioos_category | String | Time |
attribute | nitrogen_flux | long_name | String | Nitrogen Flux |
attribute | nitrogen_flux | lter_column_description | String | non-metallic element in the Periodic Table with Atomic Number 7, Atomic Weight 14.0067 |
attribute | nitrogen_flux | lter_column_name | String | Nitrogen Flux |
attribute | nitrogen_flux | lter_mscale | String | ratio |
attribute | nitrogen_flux | lter_num_type | String | real |
attribute | nitrogen_flux | lter_units | String | mg/m²/day |
attribute | nitrogen_flux | lter_units_string | String | milligramPerMeterSquaredPerDay |
attribute | nitrogen_flux | units | String | mg m-2 day-1 |
attribute | nitrogen_flux | units_conventions | String | HFR-LTER,PAL-LTER,SBC-LTER |
variable | phosphorous_flux | double | ||
attribute | phosphorous_flux | _FillValue | double | 9.969209968386869E36 |
attribute | phosphorous_flux | actual_range | double | -9998.0, 1.17 |
attribute | phosphorous_flux | column_id | long | 316 |
attribute | phosphorous_flux | column_name | String | col_316 |
attribute | phosphorous_flux | ioos_category | String | Time |
attribute | phosphorous_flux | long_name | String | Phosphorous Flux |
attribute | phosphorous_flux | lter_column_description | String | a non-metallic element in the Periodic Table with Atomic Number 15, Atomic Weight 30.973762 |
attribute | phosphorous_flux | lter_column_name | String | Phosphorus Flux |
attribute | phosphorous_flux | lter_mscale | String | ratio |
attribute | phosphorous_flux | lter_num_type | String | real |
attribute | phosphorous_flux | lter_units | String | mg/m²/day |
attribute | phosphorous_flux | lter_units_string | String | milligramPerMeterSquaredPerDay |
attribute | phosphorous_flux | units | String | mg m-2 day-1 |
attribute | phosphorous_flux | units_conventions | String | HFR-LTER,PAL-LTER,SBC-LTER |
variable | notes | String | ||
attribute | notes | column_id | long | 3855 |
attribute | notes | column_name | String | col_3855 |
attribute | notes | ioos_category | String | Unknown |
attribute | notes | long_name | String | Notes |
attribute | notes | lter_column_description | String | text field to describe a log entry (ex. event log) |
attribute | notes | lter_column_name | String | Notes |
attribute | notes | lter_mscale | String | nominal |
The information in the table above is also available in other file formats (.csv, .htmlTable, .itx, .json, .jsonlCSV1, .jsonlCSV, .jsonlKVP, .mat, .nc, .nccsv, .tsv, .xhtml) via a RESTful web service.