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Polar meteorology

A review of some recent research

Bibliographic Data

ID14437901
AuthorsGunter Weller (corresponding author)
Year1974
Volume17
Issue108
Pages277-294
Publication date1974-09-01
Open AccessYes
TypeARTICLE
VenuePolar Record (JOURNAL)
Journal identifiersISSN: 0032-2474 • E-ISSN: 1475-3057
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/s0032247400031934
OpenAlexW2127082149
LanguageEN
References cited38

The general large-scale circulation of the global atmosphere has its basic driving mechanism in the equator-poleward temperature gradients in both hemispheres. It has become increasingly obvious over the last few decades that to understand and predict the behaviour of the atmosphere at any point, it is essential to understand the behaviour of the total global fluid system. The Global Atmospheric Research Project (GARP) is an outcome of this recognition. Studies of the heat sinks (the polar regions) are therefore just as important as studies of the heat source (the equatorial regions) to understand the meteorology of the planet. Interest in polar meteorology has undergone many cyclic fluctuations, peaking during the various international polar years and, more recently, during the International Geophysical Year, 1957–58. At the present, the focus of GARP's first objective (improved extended weather forecasts) is on the tropical heat source, where convection and cloud formation and dissipation are still relatively little understood processes. However, the second GARP objective (better understanding of the physical basis of climate) requires more attention to be devoted to the cryosphere, its long-term interaction with oceans and atmosphere, and its role as an indicator of climatic change. The idea of a polar experiment (POLEX) was initially introduced by Treshnikov and others (1968) and by Borisenkov and Treshnikov (1971). A summary of the early history of POLEX was recently given by Weller and Bierly (1973). The two closely related objectives of POLEX that most directly pertain to GARP may be restated in their simplest terms as (1) a better understanding of energy transfer processes and the heat budgets of the polar regions for the purpose of parameterizing them properly in general circulation models and climate models, and (2) provision of adequate data from the polar regions during the First GARP Global Experiment (FGGE) in 1978

Atmosphere (unit) · Atmospheric sciences · Climatology · Convection · Equator · Geography · Latitude · Meteorology · Physics · Polar · Arctic and Antarctic ice dynamics · Atmospheric and Environmental Gas Dynamics · Climate variability and models · Environmental Science · Geology

  • The Tundra Microclimate During Snow-Melt at Barrow, Alaska

    Open Access•Gunter Weller•ARCTIC•1972

  • Climates of the polar regions

    Open Access•Colin Bull•Geoforum•1973

Highly citedNo

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