For the next three months severe to exceptional water deficits are forecast to persist in Cambodia, particularly in the west, and severe to extreme deficits will emerge throughout much of Thailand. Deficits are also forecast for southern Myanmar and Papua New Guinea. Both deficits and surpluses are forecast in Laos during this period and in Vietnam, though surpluses will dominate Vietnam’s central coast. After May deficits of varying intensity are forecast for much of the region and are expected to be of greatest severity in Papua New Guinea and Indonesian Borneo.
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ISciences Worldwide Water Watch List March 2017
Regions likely to have significant water deficits for the 12-month period from December 2016 through November 2017 include: Arkansas, Quebec, Brazil, Finland, Denmark, Libya, Niger, Gabon, Madagascar, Saudi Arabia, Yemen, northern Russia, Inner Mongolia, Thailand, western Cambodia, Papua New Guinea, and eastern Australia. Water surpluses are forecast for: Idaho, Central California, southwestern Zambia, the Okavango Delta in Botswana, northeastern Afghanistan, and between the Irtysh and Yenisei Rivers in Russia. This Watch List is based on ISciences Water Security Indicator Model (WSIM) Global Water Monitor and Forecast issued 8 March 2017.
Global Precipitation & Temperature Outlook for March 2017
The March 2017 Outlook indicates drier than normal conditions in southern California and eastern Brazil, and wetter than normal conditions in Venezuela, Guyana, Suriname, Paraguay, and Namibia and neighboring African nations. The forecast for many parts of the world is for much warmer than normal conditions including: Europe, Russia, Yemen, Queensland (Australia), Madagascar, Brazil, Cuba, and southwestern Mexico.
The Generational Experience
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.





