Marine Mammal sighting data from cruises in the Pacific Arctic, 2018, from Distributed Biological Observatory (DBO) regions

The Pacific Arctic region (PAR) extends from the northern Bering Sea to the Arctic Ocean Basin, and it is experiencing major reductions in seasonal sea ice and increases in sea surface temperatures. Within the PAR, the northern Bering and Chukchi Seas are among the most productive marine ecosystems...

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Main Author: Stafford, Kathleen
Format: Dataset
Language:English
Published: Arctic Data Center 2019
Subjects:
Online Access:https://dx.doi.org/10.18739/a2nv99b09
https://arcticdata.io/catalog/#view/doi:10.18739/A2NV99B09
id ftdatacite:10.18739/a2nv99b09
record_format openpolar
spelling ftdatacite:10.18739/a2nv99b09 2023-05-15T13:22:58+02:00 Marine Mammal sighting data from cruises in the Pacific Arctic, 2018, from Distributed Biological Observatory (DBO) regions Stafford, Kathleen 2019 text/xml https://dx.doi.org/10.18739/a2nv99b09 https://arcticdata.io/catalog/#view/doi:10.18739/A2NV99B09 en eng Arctic Data Center Distributed Biological Observatory DBO Marine Mammal Visual observations dataset Dataset 2019 ftdatacite https://doi.org/10.18739/a2nv99b09 2021-11-05T12:55:41Z The Pacific Arctic region (PAR) extends from the northern Bering Sea to the Arctic Ocean Basin, and it is experiencing major reductions in seasonal sea ice and increases in sea surface temperatures. Within the PAR, the northern Bering and Chukchi Seas are among the most productive marine ecosystems in the Arctic and are important carbon sinks and seasonal sources of organic materials. These recent shifts in seasonal sea ice cover are having profound consequences for seasonal phytoplankton production as well as to intimately linked higher trophic levels, including food harvested locally for subsistence. Key uncertainties remain as to how the marine ecosystem will respond to seasonal shifts in the timing of spring sea ice retreat and/or delays in fall sea ice formation. Productivity may change as sea ice declines and penetration of sunlight into open water increases, but the trajectory of changes to food web structure are unclear. Many organisms, from plankton to top predators are changing their distribution, migration and foraging patterns. A number of marine sites in the Pacific Arctic have high biomass, both in the water column and on the seafloor and are focused foraging points for apex predators. Several of these sites have been identified and re-occupied seasonally and interannually during multiple international cruises as part of the Distributed Biological Observatory (DBO) network. The DBO observational data documenting the importance of these ecosystem “hotspots” provide a growing marine time-series from the northern Bering Sea to Barrow Canyon at the boundary of the Chukchi and Beaufort seas, and across the Beaufort Sea to Amundsen Gulf. In US waters, these sites are DBO1 (south of St. Lawrence Island, DBO2 (Chirikov Basin north of SLI), DBO3 (southern Chukchi Sea), DBO4 (central Chukchi Sea), DBO5 (upper Barrow Canyon) , DBO6 (Beaufort Sea shelf break at ~152 West). As part of DBO efforts, marine mammal visual detections have been obtained from any research voyage with an on-board observer and sightings within DBO regions 1-6 have been highlighted. This dataset contains observations from the vessels: Healy, Sir Wilfrid Laurier (SWL), and Sikuliaq. Dataset Amundsen Gulf Arctic Arctic Ocean Beaufort Sea Bering Sea Chukchi Chukchi Sea Pacific Arctic Phytoplankton Sea ice St Lawrence Island DataCite Metadata Store (German National Library of Science and Technology) Arctic Arctic Ocean Barrow Canyon ENVELOPE(-154.000,-154.000,72.500,72.500) Bering Sea Chukchi Sea Lawrence Island ENVELOPE(-103.718,-103.718,56.967,56.967) Pacific
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Distributed Biological Observatory DBO
Marine Mammal
Visual observations
spellingShingle Distributed Biological Observatory DBO
Marine Mammal
Visual observations
Stafford, Kathleen
Marine Mammal sighting data from cruises in the Pacific Arctic, 2018, from Distributed Biological Observatory (DBO) regions
topic_facet Distributed Biological Observatory DBO
Marine Mammal
Visual observations
description The Pacific Arctic region (PAR) extends from the northern Bering Sea to the Arctic Ocean Basin, and it is experiencing major reductions in seasonal sea ice and increases in sea surface temperatures. Within the PAR, the northern Bering and Chukchi Seas are among the most productive marine ecosystems in the Arctic and are important carbon sinks and seasonal sources of organic materials. These recent shifts in seasonal sea ice cover are having profound consequences for seasonal phytoplankton production as well as to intimately linked higher trophic levels, including food harvested locally for subsistence. Key uncertainties remain as to how the marine ecosystem will respond to seasonal shifts in the timing of spring sea ice retreat and/or delays in fall sea ice formation. Productivity may change as sea ice declines and penetration of sunlight into open water increases, but the trajectory of changes to food web structure are unclear. Many organisms, from plankton to top predators are changing their distribution, migration and foraging patterns. A number of marine sites in the Pacific Arctic have high biomass, both in the water column and on the seafloor and are focused foraging points for apex predators. Several of these sites have been identified and re-occupied seasonally and interannually during multiple international cruises as part of the Distributed Biological Observatory (DBO) network. The DBO observational data documenting the importance of these ecosystem “hotspots” provide a growing marine time-series from the northern Bering Sea to Barrow Canyon at the boundary of the Chukchi and Beaufort seas, and across the Beaufort Sea to Amundsen Gulf. In US waters, these sites are DBO1 (south of St. Lawrence Island, DBO2 (Chirikov Basin north of SLI), DBO3 (southern Chukchi Sea), DBO4 (central Chukchi Sea), DBO5 (upper Barrow Canyon) , DBO6 (Beaufort Sea shelf break at ~152 West). As part of DBO efforts, marine mammal visual detections have been obtained from any research voyage with an on-board observer and sightings within DBO regions 1-6 have been highlighted. This dataset contains observations from the vessels: Healy, Sir Wilfrid Laurier (SWL), and Sikuliaq.
format Dataset
author Stafford, Kathleen
author_facet Stafford, Kathleen
author_sort Stafford, Kathleen
title Marine Mammal sighting data from cruises in the Pacific Arctic, 2018, from Distributed Biological Observatory (DBO) regions
title_short Marine Mammal sighting data from cruises in the Pacific Arctic, 2018, from Distributed Biological Observatory (DBO) regions
title_full Marine Mammal sighting data from cruises in the Pacific Arctic, 2018, from Distributed Biological Observatory (DBO) regions
title_fullStr Marine Mammal sighting data from cruises in the Pacific Arctic, 2018, from Distributed Biological Observatory (DBO) regions
title_full_unstemmed Marine Mammal sighting data from cruises in the Pacific Arctic, 2018, from Distributed Biological Observatory (DBO) regions
title_sort marine mammal sighting data from cruises in the pacific arctic, 2018, from distributed biological observatory (dbo) regions
publisher Arctic Data Center
publishDate 2019
url https://dx.doi.org/10.18739/a2nv99b09
https://arcticdata.io/catalog/#view/doi:10.18739/A2NV99B09
long_lat ENVELOPE(-154.000,-154.000,72.500,72.500)
ENVELOPE(-103.718,-103.718,56.967,56.967)
geographic Arctic
Arctic Ocean
Barrow Canyon
Bering Sea
Chukchi Sea
Lawrence Island
Pacific
geographic_facet Arctic
Arctic Ocean
Barrow Canyon
Bering Sea
Chukchi Sea
Lawrence Island
Pacific
genre Amundsen Gulf
Arctic
Arctic Ocean
Beaufort Sea
Bering Sea
Chukchi
Chukchi Sea
Pacific Arctic
Phytoplankton
Sea ice
St Lawrence Island
genre_facet Amundsen Gulf
Arctic
Arctic Ocean
Beaufort Sea
Bering Sea
Chukchi
Chukchi Sea
Pacific Arctic
Phytoplankton
Sea ice
St Lawrence Island
op_doi https://doi.org/10.18739/a2nv99b09
_version_ 1766368232708505600