Circumpolar Flaw Lead System Study

Measurements taken within the Cape Bathurst flaw lead on board the icebreaker C.C.G.S. Amundsen to examine how physical changes affect biological processes in the flaw lead through an entire annual cycle (October 2007 - August 2008). The circumpolar flaw lead occurs each year when the central pack ice moves away from the coastal fast ice creating an area of open water called a flaw lead.

Data and Resources

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Additional Info

Field	Value
Maintainer	undefined
Last Updated	March 31, 2025, 18:19 (UTC)
Created	March 31, 2025, 18:19 (UTC)
accessLevel	public
bureauCode	{026:00}
catalog_@context	https://project-open-data.cio.gov/v1.1/schema/catalog.jsonld
catalog_@id	https://data.nasa.gov/data.json
catalog_conformsTo	https://project-open-data.cio.gov/v1.1/schema
catalog_describedBy	https://project-open-data.cio.gov/v1.1/schema/catalog.json
citation	Archived by National Aeronautics and Space Administration, U.S. Government, NASA/GSFC/SED/ESD/GCDC/OB.DAAC. https://doi.org/10.5067/SeaBASS/CFL/DATA001.
harvest_object_id	37682961-0c1c-43be-be01-9dac04acacac
harvest_source_id	61638e72-b36c-4866-9d28-551a3062f158
harvest_source_title	DNG Legacy Data
identifier	C2131352566-OB_DAAC
issued	2008-03-24
landingPage	https://doi.org/10.5067/SeaBASS/CFL/DATA001
language	{en-US}
metadata_type	geospatial
modified	2023-04-06
programCode	{026:001}
publisher	NASA/GSFC/SED/ESD/GCDC/OB.DAAC
resource-type	Dataset
source_datajson_identifier	true
source_hash	84031bb1ede8fa7016ce8521ae3919471a2e2c635396c698223938f6e65f1ff7
source_schema_version	1.1
spatial	-180.0 -90.0 180.0 90.0
temporal	2008-03-24T00:00:02Z/2008-08-08T23:59:59Z
theme	{geospatial}