NO EVIDENCE FOR IRIS
It is shown that the negative correlation between cloud-weighted sea surface temperature (SST) and high cloud fraction discussed recently by Lindzen et al. results from variations in subtropical clouds that are not physically connected to the deep convection near the equator. A negative correlation...
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| Veröffentlicht in: | Bulletin of the American Meteorological Society 2002-02, Vol.83 (2), p.249-254 |
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| container_title | Bulletin of the American Meteorological Society |
| container_volume | 83 |
| creator | Hartmann, Dennis L. Michelsen, Marc L. |
| description | It is shown that the negative correlation between cloud-weighted sea surface temperature (SST) and high cloud fraction discussed recently by Lindzen et al. results from variations in subtropical clouds that are not physically connected to the deep convection near the equator. A negative correlation between cloud-weighted SST and average cloud fraction results from any variation in cloud fraction over the areas with lower SSTs within the domain of interest. Therefore,this correlation is not evidence that tropical cloud anvil area is inversely proportional to sea surface temperature and should not be used to infer the existence of a negative feedback in the climate system. |
| doi_str_mv | 10.1175/1520-0477(2002)083<0249:NEFI>2.3.CO;2 |
| format | Article |
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| ispartof | Bulletin of the American Meteorological Society, 2002-02, Vol.83 (2), p.249-254 |
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| source | Jstor Complete Legacy; American Meteorological Society; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals |
| subjects | Anvil clouds Cloud cover Clouds Convection Convection clouds Correlations Earth, ocean, space Exact sciences and technology External geophysics Meteorology Oceans Physics of the oceans Sea surface temperature Sea-air exchange processes Spatial analysis Subtropics Temperate regions Temperature Time series Water in the atmosphere (humidity, clouds, evaporation, precipitation) Wind |
| title | NO EVIDENCE FOR IRIS |
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