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Analysis of climate change impact on rainfall pattern of Sambas district, West Kalimantan

机译:西红梅坦斯桑巴斯区降雨模式的气候变化影响分析

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Climate change is one of the most important issues being discussed globally. It caused by global warming and indirectly affecting the world climate cycle. This research discussed the effect of climate change on rainfall pattern of Sambas District and predicted the future rainfall pattern due to climate change. CRU and TRMM were used and has been validated using in situ data. This research was used Climate Modelling and Prediction using CCAM (Conformal Cubic Atmospheric Model) which also validated by in situ data (correlation= 0.81). The results show that temperature trends in Sambas regency increased to 0.082°C/yr from 1991-2014 according to CRU data. High temperature trigger changes in rainfall patterns. Rainfall pattern in Sambas District has an equatorial type where the peak occurs when the sun is right on the equator. Rainfall in Sambas reaches the maximum in March and September when the equinox occurs. The CCAM model is used to project rainfall in Sambas District in the future. The model results show that rainfall in Sambas District is projected to increase to 0.018 mm/month until 2055 so the flow rate increase 0.006 m~3/month and the water balance increase 0.009 mm/month.
机译:气候变化是全球讨论的最重要问题之一。它由全球变暖和间接影响世界气候周期引起的。本研究探讨了气候变化对桑巴地区降雨模式的影响,并预测了由于气候变化导致的未来降雨模式。使用CRU和TRMM,并使用原位数据进行验证。使用CCAM(保形立方体大气模型)的气候建模和预测使用了该研究,该研究也通过原位数据验证(相关= 0.81)。结果表明,根据CRU数据,Sambas Regency的温度趋势从1991 - 2014年增加到0.082°C / YR。降雨模式的高温触发变化。桑巴地区的降雨模式有一个赤道类型,当太阳在赤道上就会发生峰值。桑巴的降雨量在昼夜发生时,3月和9月达到最多。 CCAM模型用于将来在桑巴地区的降雨量。模型结果表明,桑巴地区的降雨预计将增加到0.018毫米/月,直到2055年,因此流量增加0.006米〜3个月,水平增加0.009毫米/月。

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