% From
% Woodgate, R.A.,  K. Aagaard, and T.J. Weingartner (2005)
%  Monthly temperature, salinity, and transport variability
%  of the Bering Strait throughflow.
%  Geophys. Res. Lett.,
%  Vol. 32, No. 4, L04601 10.1029/2004GL021880. 2005
%
% Table 1. Climatological Near-Bottom Temperature (T),
%  Salinity (S), and Principal Component (V) of Velocity
%  (Heading 329 deg) at A3**
%
%        T (degC)      S (psu)      V (cm/s)   Vol (Sv)
 Jan   -1.77 (.01)   32.39 (.16)   11.4 (3.3)   0.4
 Feb   -1.79 (.01)   32.76 (.17)   15.3 (2.2)   0.6
 Mar   -1.80 (.01)   32.95 (.20)   18.2 (3.0)   0.7
 Apr   -1.78 (.01)   32.88 (.13)   21.7 (3.0)   0.8
 May   -1.44 (.08)   32.65 (.12)   29.5 (2.0)   1.2
 Jun   -0.06 (.20)   32.45 (.10)   32.5 (2.0)   1.3
 July  +1.59 (.30)   32.51 (.06)   29.2 (1.6)   1.1
 Aug   +2.07 (.31)   32.44 (.04)   26.8 (2.6)   1.0
 Sep   +2.25 (.27)   32.47 (.06)   18.6 (3.2)   0.7
 Oct   +2.22 (.26)   32.46 (.06)   16.1 (1.7)   0.6
 Nov   +0.62 (.35)   32.07 (.11)   18.6 (1.5)   0.7
 Dec   -1.36 (.15)   31.91 (.21)   13.1 (3.5)   0.5

 AM    -0.1  (0.2)   32.5  (0.1)   20.9 (2.5)   0.8

Estimated errors are in parentheses (grey areas on Figures 2, 3, 4, and 5).
Standard deviations (thin black lines on Figures 2, 3, 4, and 5) are ~3 times
these errors. Estimated transports (Vol) have errors ~25%. Water column
means are probably ~0.5 to 1 psu fresher and 1 to 2degC warmer than these
values during summer/autumn (~May– October). AM = annual mean.