Regional Cloud Cover Change Associated with Global Climate Change Case Studies for Three Regions of the United States

• Published in: Journal of climate Vol. 12; no. 7; pp. 2128 - 2134
• Main Authors: Croke, Meredith S., Cess, Robert D., Hameed, Sultan
• Format: Journal Article
• Language: English
• Published: Boston, MA American Meteorological Society 01-07-1999
• Subjects: Climate; Climate change; Climatic zones; Cloud cover; Clouds; Correlations; Datasets; Earth, ocean, space; Exact sciences and technology; External geophysics; Global climate; Global warming; High pressure; Low pressure; Meteorology; NOTES AND CORRESPONDENCE; Regions; Seasons; Surface temperature; Temperature; Water in the atmosphere (humidity, clouds, evaporation, precipitation); United States; North America; America; United States > US; Case study; Surface temperature; Data analysis; Clouds; Atmospheric pressure; Climate modification
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/1520-0442(1999)012<2128:RCCCAW>2.0.CO;2

Land-based observations of cloud cover, for the period 1900–87 and averaged over three geographical regions of the United States (coastal southwest, coastal northeast, and southern plains), show strong positive correlations with one estimate of global mean surface temperature, a finding consistent with prior investigations that suggest cloud cover over land has increased during global warm periods relative to cold periods. It is also found that the strengths of three permanent high/low pressure systems (North Pacific high, Icelandic low, and Azores high) are negatively correlated with global mean surface temperature, suggesting a possible connection between regional cloud cover, for certain locations, and the strengths of adjacent high/low pressure systems. Specifically, for the regions considered it is suggested that the coastal southwest cloud cover is related to changes in the strength of the subtropical North Pacific high, that for the southern plains also to the strength of the North Pacific high, and that for the coastal northeast to the strength of the Icelandic low. Thus the climate-induced change in cloud cover for certain regions appears related, at least in part, to climate-induced change in the strengths of adjacent high/low pressure systems, and plausible physical explanations for this relation are provided for the three regions that have been studied. This does not, of course, provide a direct physical cause-and-effect explanation for the changes in regional cloud cover, because the mechanisms that cause the intensities of the high/low pressure systems to change are not understood.