Surface Circulation of Lakes and Nearly Land-Locked Seas
AUTOR(ES)
Emery, K. O.
RESUMO
The pattern of surface circulation has been mapped for more than 40 lakes, marginal seas, estuaries, and lagoons. All are within the northern hemisphere, and all except one are known to have a counterclockwise pattern. This consistent pattern is attributed to the drag of wind blowing across the bodies of water. Warmer surface water is displaced to the right-hand shore zone (facing downwind), where it produces greater surface turbulence and, thus, greater wind drag. This effect leads to counterclockwise water circulation regardless of the direction and, within limits, the duration of the wind.
ACESSO AO ARTIGO
http://www.pubmedcentral.nih.gov/articlerender.fcgi?artid=433191Documentos Relacionados
- DISPOSAL OF RADIOACTIVE WASTES INTO SEAS, OCEANS AND SURFACE
- On the cyclonic mean circulation of large lakes†
- Phosphorus in Connecticut lakes predicted by land use
- A snapshot of the limnological features in tropical floodplain lakes: the relative influence of climate and land use
- The Ages of the Lunar Seas