Observed increases in Bering Strait oceanic fluxes from the Pacific to the Arctic from 2001 to 2011 and their impacts on the Arctic Ocean water columnRebecca A Woodgate, Thomas
J Weingartner and Ron Lindsay
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Please contact Rebecca Woodgate (woodgate@apl.washington.edu) for use of any of this material
AbstractMooring data indicate the Bering Strait
throughflow increases ~50% from 2001 (~0.7Sv) to 2011 (~1.1Sv),
driving heat and freshwater flux increases. Increase in the
Pacific-Arctic pressure-head explains two-thirds of the change,
the rest being attributable to weaker local winds. The 2011 heat
flux (~5x1020J) approaches the previous record high
(2007) due to transport increases and warmer lower layer (LL)
temperatures, despite surface temperature (SST) cooling. In the
last decade, warmer LL waters arrive earlier (1.6±1.1
days/yr), though winds and SST are typical for recent decades.
Maximum summer salinities, likely set in the Bering Sea, remain
remarkably constant (~33.1psu) over the decade, elucidating the
stable salinity of the western Arctic cold halocline. Despite
this, freshwater flux variability (strongly driven by transport)
exceeds variability in other Arctic freshwater sources. Remote
data (winds, SST) prove insufficient for quantifying
variability, indicating interannual change can still only be
assessed by in situ year-round measurements.
© Polar Science Center,
University of Washington, 2012
First row: All A3 lower layer (LL) data
from 1998 to 2011. Rows 2-5: A3 LL data from cold years
1991 (row 2)
and 2001 (row
3) and warm years 2007 (row 4) and
2011 (row 5).
First column: Temperature-salinity (TS)
plot with sigma-0 contours showing that year’s data
(in color) and 1998-2011 data (grey). Black box
marks extract of TS plot shown in column 2. Yellow
line is a western Arctic TS profile from 2002 (CBL2002
station 14 - 76º31.4’N, 168º51.8W in 750m
water north of the Chukchi slope [Woodgate et al., 2005c]). Second column: Volume of water (in TS
classes) for that year (or group of years) infered
from moored velocity measurements. Positive/Negative
values
indicate net northward/southward transport. Third column: Volume of
water per salinity class for that year (or group of
years) above 0ºC (red), below 0ºC (blue),
and total (black).
Grey lines indicate totals from each year
1998-2011. Fourth column: Heat flux per sigma-0 class
for that year (or group of years). Grey lines
indicate totals from each year 1998-2011. In
first 3 columns, black dashed line marks 33.1 psu. |
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