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Matrix of data collections during the multiple international cruises at one or both of the DBO sites in a pilot mode is shown below

 

2010 International DBO project cruise and contact information

Dates (2010) /Port calls

Ship

Project

PAG contact

Chief Scientist

June 15 (Dutch Harbor), July 25 (Seward)

Healy 1001

ICESCAPE (NASA)

Robert Pickart rpickart@whoi.edu

 

Kevin Arrigo Kevin.arrigo@healy.polarscience.net

 

July 6 (Victoria, BC),

July 22 (Barrow)

Sir Wilfrid Laurier

Canada’s Three Oceans (C30) (DFO)

Jackie Grebmeier

jgrebmei@umces.edu

Svein Vagle

Svein.Vagle@dfo-mpo.gc.ca

July 1 (Korea), July 23 (Barrow), Sept 10 (Nome)

Xuelong

China Arctic Expedition (CHINARE)

Jingfeng He heijianfeng@pric.gov.cn

Yu Xingguang Yu_xg@163.com, Science Lead: Jingfeng He heijianfeng@pric.gov.cn

July 1-July 23 (Nome)

Aaron

Korean Expedition

Sang Lee sanglee@kopri.re.kr

Kyungho Chung khchung@kopri.re.kr

July 24 - August 12

Moana Wave

COMIDA-Phase 1

Jackie Grebmeier

jgrebmei@umces.edu

Jackie Grebmeier

jgrebmei@umces.edu

September 2 – October 15

Mirai

 

Motoyo Itoh motoyo@jamstec.go.jp

Motoyo Itoh motoyo@jamstec.go.jp

July 31-August11 (Nome)

Khromov

RUSALCA

Kathy Crane Kathy.Crane@noaa.gov

Rebecca Woodgate woodgate@apl.washington.edu

August 23-Sept. 21 (Barrow)

Annika Marie

BOWFEST

Carin Ashjian cashjian@whoi.edu

Carin Ashjian cashjian@whoi.edu

August 24 (Nome), Sept. 8 (Barrow), Sept. 13 (Nome), Sept 20 (Dutch Harbor)

Alaskan Enterprise

 

Chukchi Acoustics, Oceanography, and Zooplankton Study (CHAOZ) (NOAA)

Sue Moore sue.moore@noaa.gov

Jeff Napp Jeff.Napp@noaa.gov

 

Catherine Berchok

Catherine.Berchok@noaa.gov Mooring lead: Tom Weingartner weingart@ims.uaf.edu

September 7-23

Healy 1003

Beaufort Sea moorings

Robert Pickart rpickart@whoi.edu,

Robert Pickart rpickart@whoi.edu,

 

DBO 3 :SE Chukchi Sea Sir Wilfrid Laurier (July) vs RV Mirai (Sept). Over the season the Alaska Coastal Current (ACC) bringing warmer water to the system in the east. In the west warming Anadyr water results in warm Chukchi Sea summer water. Within the lower panels we see the average stratification at about 20 m along the transect from west (left side of left panel) to the eastern coastal stations. By comparison, the Sept. station is nearly vertical, indicating fall mixing, resulting in an average 3 deg C temperature throughout the water column, and much more saline water with the input of more saline Anadyr water northward in the SE Chukchi Sea. Note that two other cruises occupied this line (ICESCAPE and RUSALCA) and those data sets will be updated on this figure.

 

6 occupations of the DBO 4 (Barrow Canyon) line by 4 countries (US, Canada, China and Japan)
There were 6 occupations of the DBO 4 (Barrow Canyon) line by 4 countries (US, Canada, China and Japan).

 

Barrow Canyon potential temperature (c).
Individual Sections: Potential Temperature (C). In Barrow Canyon the Alaska Coastal Current is warmest along the Alaska coast in early September.

 

Barrow Canyon salinity.
Individual Sections: Salinity. Barrow Canyon the Bering Sea winter water is saltiest early in the season, entering the canyon on the western side.

 

Barrow Canyon lnitrates.

In Barrow Canyon Bering Shelf water is highest in nitrate late in the season in bottom waters, with the surface waters having been stripped by primary producers earlier in the season [note other time series nutrients, chlorophyll, prey and predator data coming soon]

 

Barrow Canyon lnitrates.

In upper Barrow Canyon, in 2010 spring bloom occurs in May (also see Hill et al. 2005 for earlier times series in this area). In recent years a later, stronger fall bloom is occurring in October.