Year Established: 2014 Start Date: 2014-03-01 End Date: 2015-02-28
Total Federal Funds: $15,106 Total Non-Federal Funds: Not available
Principal Investigators: Mark Lander, Shahram Khosrowpanah
Abstract: Problem: All states of the FSM are vulnerable to damaging drought conditions, despite high average annual rainfall amounts (e.g.,Yap Island = 120 inches, Chuuk Airport = 135 inches, Kolonia, Pohnpei = 185 inches, and Kosrae Airport = 205 inches). In the first few months of the calendar year that follows a strong El Nithe rainfall across all of Micronesia tends to be well below normal. Sharply reduced rainfall can quickly become a life-threatening emergency as reservoirs and rain catchment systems run dry, and agricultural plants are damaged. This is especially true on atolls where the water lenses are thin and rain catchment is a prominent source of drinking water. Micronesia-wide severe droughts in 1983, 1992 and 1998 required the deployment of U.S. military assets to the islands of the FSM to help transport and generate drinking water supplies. Recently, a more localized severe drought occurred in the northern atolls of the Republic of the Marshall Islands. This drought was so severe over the first few months of 2013 that on 14 June, U.S. President Obama declared a disaster for the RMI, authorizing additional U.S. Government funding for relief and reconstruction. Another recent local severe drought occurred on the atoll of Kapingamarngi (Pohnpei State) where rainfall during the six-month period beginning in September 2010 through February 2011 was only 7.12 inches, or 7% of the normal 48.37 inches. These dry conditions at Kapingamarangi and at other islands close to the equator (e.g., Tarawa and Nauru) are thought to have occurred because of a La Nielated westward extension of cold sea surface temperatures along the equator. Small personal distillation units from government and non-government sources and reliable water shipments by the FSM and Pohnpei State governments averted a likely disaster. Since widespread drought across the FSM typically follows a strong El Niit is therefore potentially foreseeable a few months in advance. Regional severe droughts are harder to anticipate and their causes are not well established. Another factor to consider is a statistically significant drying trend from most locations from Chuuk State eastward to the RMI (and across most of Hawaii!) in the nearly 65-year post WW II historical record. Each of the four states of the FSM has at least one nearly complete long-term (65-year) climate record. Efforts by the respective local weather offices have yielded many shorter records at outer island locations that are now approaching 15 years (or more) of continuous climate data with at least monthly resolution. An evaluation of rainfall variability and drought thresholds for atolls and high islands of the FSM directly relates to stated water quantity problems, FSM advisory meeting, October 2013. Objectives: The objectives of this project are to:(1) compile as much of the FSM climate record as possible from the first order stations and the growing network of outer island stations,(2) analyze the climate records to provide a detailed picture of El Nielated drought, and the nature of more localized droughts, (3) establish impact thresholds during periods of reduced rainfall, and (4) develop an outreach itinerary for group discussion of drought during FSM visits.