The influence of pre‐existing soil moisture content on Australian winter climate

We have performed some experiments with the University of Melbourne General Circulation Model to determine the transient response of the climate system to the imposition of soil moisture anomalies over the Australian continent. Two sets of cases have been performed in which the soil over the entire continent was saturated and was completely dried on the first day of winter and then allowed to evolve normally for 4 months. The evaporation over most of the Australian continent in the ‘saturated’ case initially was significantly greater than that in the mean and this situation persisted for the 4 month's duration of the experiments, into the spring. A similar statement is true for the reduction of evaporation in the ‘dry’ experiments, although the magnitude was not as great. As dictated by surface energy considerations, the sensible heat fluxes over most of Australia assumed signs opposite to those of the evaporation and magnitudes somewhat smaller, but the residual differences were still significant in September. Other atmospheric parameters, such as precipitation, surface temperature and mean sea-level pressure tend to show much less persistence when averaged over Australia as a whole. However, many regions do show longer influence of the perturbed initial conditions. Of considerable interest to the value of Australian winter and spring crops is the finding that the soil moisture content still showed significant anomalies persisting into the fourth month, with an areal mean of 2.7 cm more than the control in the ‘wet’ case and 1.5 cm less in the ‘dry’. This persistence of, albeit exaggerated, initial anomalies of winter soil moisture suggests that early winter soil moisture conditions may hold some potential for forecasting Australian winter crop productivity. We have found the ‘halving time’ of these large-scale soil moisture anomalies to be about 2 months and somewhat longer at higher latitudes. These findings are consistent with many other studies and are encouraging in that most of Australia's wheat is grown in that part of the continent.

[1]  G. Meehl,et al.  A Comparison of Soil-Moisture Sensitivity in Two Global Climate Models , 1988 .

[2]  Richard W. Reynolds,et al.  A Real-Time Global Sea Surface Temperature Analysis , 1988 .

[3]  B. Hunt A model study of some aspects of soil hydrology relevant to climatic modelling , 1985 .

[4]  Ann Henderson-Sellers,et al.  Modelling tropical deforestation: A study of GCM land-surface parametrizations , 1988 .

[5]  T. N. Palmer,et al.  Response of two atmospheric general circulation models to sea-surface temperature anomalies in the tropical East and West Pacific , 1984, Nature.

[6]  R. M. Mitchell,et al.  Atmospheric and viewing angle correction of vegetation indices and grassland fuel moisture content derived from NOAA/AVHRR , 1990 .

[7]  Y. Serafini The time scale of land surface hydrology in response to initial soil moisture anomalies : a case study , 1990 .

[8]  D. Rind,et al.  The Influence of Ground Moisture Conditions in North America on Summer Climate as Modeled in the GISS GCM , 1982 .

[9]  Julia Walker,et al.  The effect of soil moisture on circulation and rainfall in a tropical model , 1977 .

[10]  Eugenia Kalnay,et al.  Global Numerical Weather Prediction at the National Meteorological Center , 1990 .

[11]  John R. Hummel,et al.  A Global Surface Albedo Model , 1979 .

[12]  Syukuro Manabe,et al.  The influence of potential evaporation on the variabilities of simulated soil wetness and climate , 1988 .

[13]  I. Simmonds,et al.  The Association of Australian Winter Climate with Ocean Temperatures to the West , 1991 .

[14]  S. Idso A note on some recently proposed mechanisms of genesis of deserts , 1977 .

[15]  P. Rowntree,et al.  Simulations of the Saharan atmosphere—dependence on moisture and albedo , 1986 .

[16]  Y. Sud,et al.  A GCM Simulation Study of the Influence of Saharan Evapotranspiration and Surface-Albedo Anomalies on July Circulation and Rainfall , 1988 .

[17]  Y. Sud,et al.  Influence of evaporation in semi‐arid regions on the July circulation: A numerical study , 1984 .

[18]  F. S. Nakayama,et al.  The Dependence of Bare Soil Albedo on Soil Water Content. , 1975 .

[19]  B. Hunt,et al.  Diurnally varying regional climatic simulations , 1989 .

[20]  Y. Sud,et al.  A study of the influence of surface albedo on July circulation in semi‐arid regions using the glas GCM , 1982 .

[21]  Ian Simmonds,et al.  Analysis of the “Spinup” of a general circulation model , 1985 .

[22]  Y. Mintz,et al.  A global monthly climatology of soil moisture and water balance , 1992 .

[23]  J. Shukla,et al.  Influence of Land-Surface Evapotranspiration on the Earth's Climate , 1982, Science.

[24]  Piers J. Sellers,et al.  A Review of Satellite Data Algorithms for Studies of the Land Surface , 1990 .

[25]  A. Kitoh,et al.  Influence of Soil Moisture and Surface Albedo Changes over the African Tropical Rain Forest on Summer Climate: Investigated with the MRI⋅GCM-I@@@MRI•GCM-Iによる数値実験 , 1988 .

[26]  B. Hunt,et al.  Interannual variability of the simulated hydrology in a climatic model-implications for drought , 1987 .

[27]  Jack Kornfield,et al.  A Comparative Study of the Effects of Albedo Change on Drought in Semi-Arid Regions. , 1977 .

[28]  Syukuro Manabe,et al.  The Effect of Soil Moisture on the Short-Term Climate and Hydrology Change—A Numerical Experiment , 1984 .

[29]  C. Priestley,et al.  On the Assessment of Surface Heat Flux and Evaporation Using Large-Scale Parameters , 1972 .

[30]  J. Deardorff A Parameterization of Ground-Surface Moisture Content for Use in Atmospheric Prediction Models , 1977 .

[31]  P. S. Eagleson,et al.  A one-dimensional interactive soil-atmosphere model for testing formulations of surface hydrology , 1990 .

[32]  Paul T. Schickedanz,et al.  The Effect of Irrigation on Warm Season Precipitation in the Southern Great Plains. , 1984 .

[33]  Neville Nicholls,et al.  Towards the prediction of major Australian droughts. , 1985 .

[34]  S. Idso,et al.  The utility of surface temperature measurements for the remote sensing of surface soil water status , 1975 .

[35]  P. Rowntree,et al.  Simulation of the atmospheric response to soil moisture anomalies over Europe , 1983 .

[36]  J. Charney Dynamics of deserts and drought in the Sahel , 1975 .