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V. Korzoun, A. Sokolov (1978)
World water balance and water resources of the earth
P. Eagleson (1982)
Land surface processes in atmospheric general circulation models : papers presented at the World Climate Research Programme study conference, held under the auspices of the WMO/ICSO [i.e. WMO/ICSU] Joint Scientific Committee in Greenbelt, Maryland, 5 to 10 January, 1981
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Micrometeorological characteristics of the 1976 hot spellMet. Mag., 108
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An investigation of surface albedo variations during the recent Sahel droughtJournal of Applied Meteorology, 18
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The Dependence of Bare Soil Albedo on Soil Water Content.Journal of Applied Meteorology, 14
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United Kingdom Meteorological Office five‐level general circulation modelMethods in Computational Physics, 17
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Julia Walker, P. Rowntree (1977)
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Positive and negative anomalies in the initial soil moisture over central Europe were introduced in turn into integrations of a global model of the July atmosphere. The results show that by modifying the partitioning of the turbulent fluxes such anomalies can have major effects on the modelled rainfall, humidity and temperature during the following 50 days over the anomaly area and that the anomalies can propagate into adjacent land areas. Similar results were obtained with a lower‐resolution version of the model. The effects on rainfall were already important on day 3 of the integration over the anomaly area and on day 6 over parts of Scandinavia outside the anomaly area. The experiment was repeated with a version of the model in which the prevailing flow over Europe was less weak with increased moist westerly flow from the Atlantic. In this case the dry anomaly persisted for only about 20 days before it became too weak to affect the evaporation significantly.
The Quarterly Journal of the Royal Meteorological Society – Wiley
Published: Jul 1, 1983
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