Loading…

Freshwater transport from the Pacific to the Bering Sea through Amukta Pass

Flow through the Aleutian Passes connects the North Pacific to the Bering Sea and ultimately the Arctic. Moorings spanning the width of Amukta Pass, deployed 2001–2008, allow quantitative assessment of volume and freshwater transports. Volume transport through Amukta Pass averages 4.7 Sv, with maxim...

Full description

Saved in:
Bibliographic Details
Published in:Geophysical research letters 2009-07, Vol.36 (14), p.L14608-n/a
Main Authors: Ladd, Carol, Stabeno, Phyllis J.
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-a5292-5e2d94fa7d270c45e473aa3b9d45c31677b776152d4f6814751844853c13a8b03
cites cdi_FETCH-LOGICAL-a5292-5e2d94fa7d270c45e473aa3b9d45c31677b776152d4f6814751844853c13a8b03
container_end_page n/a
container_issue 14
container_start_page L14608
container_title Geophysical research letters
container_volume 36
creator Ladd, Carol
Stabeno, Phyllis J.
description Flow through the Aleutian Passes connects the North Pacific to the Bering Sea and ultimately the Arctic. Moorings spanning the width of Amukta Pass, deployed 2001–2008, allow quantitative assessment of volume and freshwater transports. Volume transport through Amukta Pass averages 4.7 Sv, with maximum transport in January, minimum in September, and a secondary maximum in July. Average freshwater transport through Amukta Pass is ∼5800 km3 yr−1 with a seasonal cycle similar to that of volume transport. Combining this estimate with first‐order estimates of freshwater transports in the other eastern passes in the Aleutian chain suggests that total freshwater transport is more than five times the cross‐shelf flux of freshwater needed to supply transport through Bering Strait into the Arctic. Ongoing measurements in the Aleutian Passes are critical to understanding the influence of these waters on the Bering Sea and the Arctic Ocean.
doi_str_mv 10.1029/2009GL039095
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_crossref_primary_10_1029_2009GL039095</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1642271044</sourcerecordid><originalsourceid>FETCH-LOGICAL-a5292-5e2d94fa7d270c45e473aa3b9d45c31677b776152d4f6814751844853c13a8b03</originalsourceid><addsrcrecordid>eNqFkUFPGzEQha2qlUhpb9y7QkLqoduO7fF6fYSopBVRQS0VvVkTx5ssbLKpvSvg3-N0EUUc4DQz8veenmcY2-PwmYMwXwSAmUxBGjDqFRtxg5iXAPo1G6WX1Atd7LC3MV4CgATJR-zkOPi4vKbOh6wLtI6bNnRZFdpV1i19dkaurmqXde2_8ciHer3IfnlKY2j7xTI7XPVXHSUwxnfsTUVN9O_v6y77ffz1fPwtn55Ovo8PpzkpYUSuvJgbrEjPhQaHyqOWRHJm5qic5IXWM60LrsQcq6LkqBUvEUslHZdUzkDuso-D7ya0f3sfO7uqo_NNQ2vf9tHyAoXQHBBfRhVyBCHU1nX_CXrZ9mGdPmJLNFIWnJcJ-jRALrQxBl_ZTahXFG4tB7u9gX18g4Qf3HtSdNRUacGujg8awUsjudKJEwN3XTf-9llPO_k5FdvtJFE-iOrY-ZsHEYUrW2iplb34MbHFxcmfs_Mx2m2YDwNPi_5_hMdx7wByuqmZ</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>849336118</pqid></control><display><type>article</type><title>Freshwater transport from the Pacific to the Bering Sea through Amukta Pass</title><source>Wiley Online Library</source><source>Wiley-Blackwell AGU Digital Archive</source><creator>Ladd, Carol ; Stabeno, Phyllis J.</creator><creatorcontrib>Ladd, Carol ; Stabeno, Phyllis J.</creatorcontrib><description>Flow through the Aleutian Passes connects the North Pacific to the Bering Sea and ultimately the Arctic. Moorings spanning the width of Amukta Pass, deployed 2001–2008, allow quantitative assessment of volume and freshwater transports. Volume transport through Amukta Pass averages 4.7 Sv, with maximum transport in January, minimum in September, and a secondary maximum in July. Average freshwater transport through Amukta Pass is ∼5800 km3 yr−1 with a seasonal cycle similar to that of volume transport. Combining this estimate with first‐order estimates of freshwater transports in the other eastern passes in the Aleutian chain suggests that total freshwater transport is more than five times the cross‐shelf flux of freshwater needed to supply transport through Bering Strait into the Arctic. Ongoing measurements in the Aleutian Passes are critical to understanding the influence of these waters on the Bering Sea and the Arctic Ocean.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2009GL039095</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: American Geophysical Union</publisher><subject>Aleutian passes ; Amukta Pass ; Assessments ; Bering Sea ; Continental shelf and slope processes ; Descriptive and regional oceanography ; Earth sciences ; Earth, ocean, space ; Estimates ; Exact sciences and technology ; Flux ; freshwater transport ; Freshwaters ; Geophysics ; Moorings ; Oceanography ; Physical and chemical properties of seawater ; Time series experiments ; Transport</subject><ispartof>Geophysical research letters, 2009-07, Vol.36 (14), p.L14608-n/a</ispartof><rights>2008 American Geophysical Union</rights><rights>Copyright 2009 by the American Geophysical Union.</rights><rights>2009 INIST-CNRS</rights><rights>This paper is not subject to U.S. copyright. Published in 2009 by the American Geophysical Union</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a5292-5e2d94fa7d270c45e473aa3b9d45c31677b776152d4f6814751844853c13a8b03</citedby><cites>FETCH-LOGICAL-a5292-5e2d94fa7d270c45e473aa3b9d45c31677b776152d4f6814751844853c13a8b03</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2009GL039095$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2009GL039095$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>315,786,790,11541,27957,27958,46503,46927,50923,51032</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=21893157$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Ladd, Carol</creatorcontrib><creatorcontrib>Stabeno, Phyllis J.</creatorcontrib><title>Freshwater transport from the Pacific to the Bering Sea through Amukta Pass</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>Flow through the Aleutian Passes connects the North Pacific to the Bering Sea and ultimately the Arctic. Moorings spanning the width of Amukta Pass, deployed 2001–2008, allow quantitative assessment of volume and freshwater transports. Volume transport through Amukta Pass averages 4.7 Sv, with maximum transport in January, minimum in September, and a secondary maximum in July. Average freshwater transport through Amukta Pass is ∼5800 km3 yr−1 with a seasonal cycle similar to that of volume transport. Combining this estimate with first‐order estimates of freshwater transports in the other eastern passes in the Aleutian chain suggests that total freshwater transport is more than five times the cross‐shelf flux of freshwater needed to supply transport through Bering Strait into the Arctic. Ongoing measurements in the Aleutian Passes are critical to understanding the influence of these waters on the Bering Sea and the Arctic Ocean.</description><subject>Aleutian passes</subject><subject>Amukta Pass</subject><subject>Assessments</subject><subject>Bering Sea</subject><subject>Continental shelf and slope processes</subject><subject>Descriptive and regional oceanography</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Estimates</subject><subject>Exact sciences and technology</subject><subject>Flux</subject><subject>freshwater transport</subject><subject>Freshwaters</subject><subject>Geophysics</subject><subject>Moorings</subject><subject>Oceanography</subject><subject>Physical and chemical properties of seawater</subject><subject>Time series experiments</subject><subject>Transport</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><recordid>eNqFkUFPGzEQha2qlUhpb9y7QkLqoduO7fF6fYSopBVRQS0VvVkTx5ssbLKpvSvg3-N0EUUc4DQz8veenmcY2-PwmYMwXwSAmUxBGjDqFRtxg5iXAPo1G6WX1Atd7LC3MV4CgATJR-zkOPi4vKbOh6wLtI6bNnRZFdpV1i19dkaurmqXde2_8ciHer3IfnlKY2j7xTI7XPVXHSUwxnfsTUVN9O_v6y77ffz1fPwtn55Ovo8PpzkpYUSuvJgbrEjPhQaHyqOWRHJm5qic5IXWM60LrsQcq6LkqBUvEUslHZdUzkDuso-D7ya0f3sfO7uqo_NNQ2vf9tHyAoXQHBBfRhVyBCHU1nX_CXrZ9mGdPmJLNFIWnJcJ-jRALrQxBl_ZTahXFG4tB7u9gX18g4Qf3HtSdNRUacGujg8awUsjudKJEwN3XTf-9llPO_k5FdvtJFE-iOrY-ZsHEYUrW2iplb34MbHFxcmfs_Mx2m2YDwNPi_5_hMdx7wByuqmZ</recordid><startdate>200907</startdate><enddate>200907</enddate><creator>Ladd, Carol</creator><creator>Stabeno, Phyllis J.</creator><general>American Geophysical Union</general><general>Blackwell Publishing Ltd</general><general>John Wiley &amp; Sons, Inc</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>200907</creationdate><title>Freshwater transport from the Pacific to the Bering Sea through Amukta Pass</title><author>Ladd, Carol ; Stabeno, Phyllis J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a5292-5e2d94fa7d270c45e473aa3b9d45c31677b776152d4f6814751844853c13a8b03</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Aleutian passes</topic><topic>Amukta Pass</topic><topic>Assessments</topic><topic>Bering Sea</topic><topic>Continental shelf and slope processes</topic><topic>Descriptive and regional oceanography</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Estimates</topic><topic>Exact sciences and technology</topic><topic>Flux</topic><topic>freshwater transport</topic><topic>Freshwaters</topic><topic>Geophysics</topic><topic>Moorings</topic><topic>Oceanography</topic><topic>Physical and chemical properties of seawater</topic><topic>Time series experiments</topic><topic>Transport</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ladd, Carol</creatorcontrib><creatorcontrib>Stabeno, Phyllis J.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>Materials Science &amp; Engineering Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central</collection><collection>Advanced Technologies &amp; Aerospace Database‎ (1962 - current)</collection><collection>ProQuest Agriculture &amp; Environmental Science Database</collection><collection>ProQuest Central Essentials</collection><collection>AUTh Library subscriptions: ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aerospace Database</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection (Proquest) (PQ_SDU_P3)</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>ProQuest research library</collection><collection>ProQuest Science Journals</collection><collection>ProQuest Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>ProQuest Advanced Technologies &amp; Aerospace Database</collection><collection>ProQuest Advanced Technologies &amp; Aerospace Collection</collection><collection>Environmental Science Database</collection><collection>ProQuest Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ladd, Carol</au><au>Stabeno, Phyllis J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Freshwater transport from the Pacific to the Bering Sea through Amukta Pass</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2009-07</date><risdate>2009</risdate><volume>36</volume><issue>14</issue><spage>L14608</spage><epage>n/a</epage><pages>L14608-n/a</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><notes>ark:/67375/WNG-6WKXPTC4-5</notes><notes>ArticleID:2009GL039095</notes><notes>Tab-delimited Table 1.</notes><notes>istex:3B7032E4AB1E23FDF32B120C45BA50DDE7929440</notes><notes>ObjectType-Article-1</notes><notes>SourceType-Scholarly Journals-1</notes><notes>ObjectType-Feature-2</notes><notes>content type line 23</notes><abstract>Flow through the Aleutian Passes connects the North Pacific to the Bering Sea and ultimately the Arctic. Moorings spanning the width of Amukta Pass, deployed 2001–2008, allow quantitative assessment of volume and freshwater transports. Volume transport through Amukta Pass averages 4.7 Sv, with maximum transport in January, minimum in September, and a secondary maximum in July. Average freshwater transport through Amukta Pass is ∼5800 km3 yr−1 with a seasonal cycle similar to that of volume transport. Combining this estimate with first‐order estimates of freshwater transports in the other eastern passes in the Aleutian chain suggests that total freshwater transport is more than five times the cross‐shelf flux of freshwater needed to supply transport through Bering Strait into the Arctic. Ongoing measurements in the Aleutian Passes are critical to understanding the influence of these waters on the Bering Sea and the Arctic Ocean.</abstract><cop>Washington, DC</cop><pub>American Geophysical Union</pub><doi>10.1029/2009GL039095</doi><tpages>6</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0094-8276
ispartof Geophysical research letters, 2009-07, Vol.36 (14), p.L14608-n/a
issn 0094-8276
1944-8007
language eng
recordid cdi_crossref_primary_10_1029_2009GL039095
source Wiley Online Library; Wiley-Blackwell AGU Digital Archive
subjects Aleutian passes
Amukta Pass
Assessments
Bering Sea
Continental shelf and slope processes
Descriptive and regional oceanography
Earth sciences
Earth, ocean, space
Estimates
Exact sciences and technology
Flux
freshwater transport
Freshwaters
Geophysics
Moorings
Oceanography
Physical and chemical properties of seawater
Time series experiments
Transport
title Freshwater transport from the Pacific to the Bering Sea through Amukta Pass
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-09-22T15%3A40%3A01IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Freshwater%20transport%20from%20the%20Pacific%20to%20the%20Bering%20Sea%20through%20Amukta%20Pass&rft.jtitle=Geophysical%20research%20letters&rft.au=Ladd,%20Carol&rft.date=2009-07&rft.volume=36&rft.issue=14&rft.spage=L14608&rft.epage=n/a&rft.pages=L14608-n/a&rft.issn=0094-8276&rft.eissn=1944-8007&rft.coden=GPRLAJ&rft_id=info:doi/10.1029/2009GL039095&rft_dat=%3Cproquest_cross%3E1642271044%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a5292-5e2d94fa7d270c45e473aa3b9d45c31677b776152d4f6814751844853c13a8b03%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=849336118&rft_id=info:pmid/&rfr_iscdi=true