The forecast indicates that extreme to exceptional surpluses in northern Australia will diminish, though will still remain present in some regions of Northern Territory. Exceptional deficits across the continent will similarly dissipate, though severe deficits are expected along the southern coast of Victoria.
The forecast indicates that exceptional deficits will persist in northwestern China, southwestern Mongolia, and in the Yangtze River Basin. Surpluses of severe to exceptional intensity are expected to appear in western, southern, and northeastern regions of China.
The forecast indicates that extreme to exceptional surpluses will persist throughout India and Nepal. Exceptional deficits will expand throughout regions of Afghanistan and Pakistan.
The forecast indicates that exceptional deficits will occur in southwestern states, as well as in some areas of the Midwest. Severe to exceptional surpluses will linger in southern regions of Florida and in much of the noncontiguous U.S.
We are experiencing the warmest weather patterns recorded in the modern record. Do our grandchildren think it is warmer than usual? Would our grandparents have felt that it was generally colder during their lifetime? Can we quantify their generational experience? An analysis of three overlapping statistical baselines allows comparison of three climatological periods, 1910 to 1970, 1930 to 1990, and 1950 to 2010.
More intense precipitation events are occurring worldwide in both dry and wet climates. What has changed is the overall temperature constraint in the system. When the globe is warmer, there is more energy to work with. More heat - that is, more energy - begets more intense precipitation, and the possibility of more floods and more droughts. The most immediate threats of warming result from the changing risks of extreme weather. Unlike sea level rise which is real but less perceptible, this influence is already upon us and apparent.
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