Tolentino Pamela Louise M, Poortinga Ate, Kanamaru Hideki, Keesstra Saskia, Maroulis Jerry, David Carlos Primo C, Ritsema Coen J
National Institute of Geological Sciences, University of the Philippines, Diliman, Quezon City, Philippines 1101.
Soil Physics and Land Management (SLM), Wageningen University and Research Center, P.O. Box 47, 6700 AA Wageningen, The Netherlands.
PLoS One. 2016 Oct 17;11(10):e0163941. doi: 10.1371/journal.pone.0163941. eCollection 2016.
The Philippines is one of the most vulnerable countries in the world to the potential impacts of climate change. To fully understand these potential impacts, especially on future hydrological regimes and water resources (2010-2050), 24 river basins located in the major agricultural provinces throughout the Philippines were assessed. Calibrated using existing historical interpolated climate data, the STREAM model was used to assess future river flows derived from three global climate models (BCM2, CNCM3 and MPEH5) under two plausible scenarios (A1B and A2) and then compared with baseline scenarios (20th century). Results predict a general increase in water availability for most parts of the country. For the A1B scenario, CNCM3 and MPEH5 models predict an overall increase in river flows and river flow variability for most basins, with higher flow magnitudes and flow variability, while an increase in peak flow return periods is predicted for the middle and southern parts of the country during the wet season. However, in the north, the prognosis is for an increase in peak flow return periods for both wet and dry seasons. These findings suggest a general increase in water availability for agriculture, however, there is also the increased threat of flooding and enhanced soil erosion throughout the country.
菲律宾是世界上最易受气候变化潜在影响的国家之一。为了全面了解这些潜在影响,特别是对未来水文状况和水资源(2010 - 2050年)的影响,对菲律宾主要农业省份的24个流域进行了评估。利用现有的历史插值气候数据进行校准后,STREAM模型被用于评估在两种合理情景(A1B和A2)下,来自三个全球气候模型(BCM2、CNCM3和MPEH5)的未来河流量,然后与基线情景(20世纪)进行比较。结果预测该国大部分地区的水资源可利用量将普遍增加。对于A1B情景,CNCM3和MPEH5模型预测大多数流域的河流量和河流量变异性总体增加,流量幅度和变异性更高,而在雨季,该国中部和南部的洪峰流量重现期预计会增加。然而,在北部,预计干湿季的洪峰流量重现期都会增加。这些发现表明农业用水的可利用量总体增加,然而,全国范围内洪水威胁增加以及土壤侵蚀加剧的情况也会出现。