Jp. Dodd et In. James, DIAGNOSING THE GLOBAL HYDROLOGICAL CYCLE FROM ROUTINE ATMOSPHERIC ANALYSES, Quarterly Journal of the Royal Meteorological Society, 122(535), 1996, pp. 1475-1499
This paper discusses the extent to which atmospheric analyses produced
routinely by forecasting centres can be used to diagnose the global h
ydrological cycle. These analyses directly represent the storage and l
arge-scale advection of water vapour through a combination of observat
ions and a short model forecast. In this work, the analyses produced b
y the European Centre for Medium-Range Weather Forecasts are used. Due
to changes in the model formulation, which have a profound effect on
the analyses, only results from three years of these initialized analy
ses are presented. The equations representing the conservation of wate
r and water vapour in the atmosphere are derived and discussed, includ
ing consideration of the approximations commonly made. Diagnostics of
the storage and transport of water vapour have been calculated. The re
sults are qualitatively similar to diagnostics from other sources. In
addition, with regard to attempts to derive a global relationship betw
een the surface specific humidity and the total column water vapour, s
pecial consideration is given to the variations in the vertical distri
bution of water vapour. The profile of water vapour is found to be ver
y sensitive to the competing processes responsible for the water balan
ce in the atmosphere. Although surface fluxes of water cannot be direc
tly derived from these analyses, a technique is introduced which puts
a lower bound on the evaporation and precipitation that would be consi
stent with the analyses. The results of this technique are rather enco
uraging, and comparisons with other climatologies of surface water flu
xes could provide another way of validating these atmospheric analyses
. A diagnostic characterizing the time scale of the the small-scale pr
ocesses responsible for surface evaporation and precipitation is also
introduced. This time-scale is found to vary widely but is of the orde
r of one day where variability in the hydrological cycle is important.