Zobrazeno 1 - 10
of 35
pro vyhledávání: '"J. R. Milford"'
Publikováno v:
International Journal of Remote Sensing. 14:2695-2711
Abstract. Satellite data are routinely used to monitor the growing season over the Sahelian zone of Africa. This study seeks to relate the vegetation indices and the rainfall estimates, both derived from meteorological satellites, to help monitor and
Publikováno v:
Hydrological Processes. 5:261-270
Meteosat data for 1986 to 1988 have been used to estimate the daily rainfall over catchments of tributaries of the river Senegal in Mail and Guinea. The technique uses the methodology of the TAMSAT group of the University of Reading, which involves t
Publikováno v:
Philosophical Transactions of the Royal Society of London. B, Biological Sciences. 328:705-717
Since 1975, the Food and Agriculture Organization of the United Nations (FAO) has been pioneering the development of the use of satellite remote sensing techniques for improving the surveillance and forecasting capabilities of the centralized Desert
Autor:
G. Dugdale, J. R. Milford
Publikováno v:
Philosophical Transactions of the Royal Society of London. B, Biological Sciences. 328:689-704
Of all climatic parameters, rainfall has the greatest variability in space as well as time. It also has the greatest influence on the breeding and behaviour of migrant pests, supplying the moisture needed both for their development and for the growth
Autor:
J. R. Milford
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 118:413-414
Autor:
J. R. Milford
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 116:775-775
Autor:
S. Abdulla, W. H. Moores, S. J. Caughey, C. J. Readings, W. B. Johnston, D. A. Mansfield, J. R. Milford, T. H. Guymer
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 105:397-421
During August 1974 the Co-operative Atmospheric Boundary Layer Experiment (CABLE) took place in which several experimental groups combined resources to study spatial and temporal characteristics of the convective atmospheric boundary layer over a fai