Mc. Serreze et al., THE DISTRIBUTION AND TRANSPORT OF ATMOSPHERIC WATER-VAPOR OVER THE ARCTIC BASIN, International journal of climatology, 15(7), 1995, pp. 709-727
A comprehensive rawinsonde archive, comprising atmospheric soundings f
rom fixed stations, ships, and the former Soviet Union 'North Pole' se
ries of drifting ice stations, is used to examine features of the dist
ribution and transport of Arctic water vapour. Results are based on an
alysis of climatological, gridded seasonal and monthly fields north of
65 degrees N of precipitable water, vertically integrated vapour flux
es, and profiles of specific humidity, vapour fluxes, temperature, and
winds, compiled from objective interpolation of the quality controlle
d soundings. Emphasis is placed on contrasting conditions for winter a
nd summer, with due attention paid to the potential effects of uncerta
inties in the rawinsonde humidity data. For zonal means, specific humi
dity for all seasons typically displays a surface maximum, decreasing
poleward at all levels. Precipitable water (surface-300 hPa), has wint
er values ranging from 3 . 8 mm for 65 degrees-70 degrees N and 1 . 8
mm for 80 degrees-90 degrees N, with annual maxima in July of 18 . 2 a
nd 12 . 5 mm, respectively. These zonal means, however, mask large spa
tial variations; precipitable water for winter, spring, and autumn sho
ws a marked equatorward increase towards the Atlantic side of the Arct
ic only. Minima are found over north-east Canada during spring, summer
, and autumn. Vapour fluxes tend to peak in the lower troposphere at a
bout 850 hPa in winter, but over a broader layer in summer. During win
ter, the largest vertically integrated (surface-300 hPa) zonal and mer
idional vapour transports are found between Iceland and Scandinavia. T
he Beaufort Sea and western Canada are the only regions where vertical
ly integrated meridional fluxes are equatorward. During summer, the ve
rtically integrated total flux (zonal plus meridional components) incr
eases sharply over the Beaufort Sea. Equatorward meridional fluxes are
again found over western Canada, with strong poleward meridional tran
sports over the Atlantic sector.