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The effect of climate change on solar radiation in Nigeria

机译:气候变化对尼日利亚太阳辐射的影响

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In this study, global solar radiation over Nigeria was simulated under an enhanced atmospheric CO2 level using the International Centre for Theoretical Physics (ICTP) Regional Climate Model version 3 (RegCM3) for the period 1981 to 2100 with ECHAM5 GCM as the lateral boundary conditions. The simulated seasonal global solar radiation bias for the RegCM3 with NIMET and NASA observed datasets in the control period are of similar magnitudes and showed a mixture of persistent positive and negative biases ranging between -10% and 30%. The model generally underestimates solar radiation (biases -10% to -30%) across the whole country in most of the months. In addition, it overestimates radiation (biases +2-30%) over the northern region of the country. Alongside the present climate (1981-2010), three future periods were considered viz: period 1 (2011-2040), period 2 (2041-2070) and period 3 (2071-2100) for the potential future changes. The seasonal potential future changes in period 1 (i.e. potential future changes with respect to 2040) showed a reduction in the range of 0% (North) to 3.27% (South) whereas more reduction in global solar radiation is observed in period 2 (i.e. 2041-2070 minus present climate) having general decrease ranging from 0.11% to 3.39% with the least value in April (Middle-belt) and the largest in the South zone (March). Potential future changes in period 3 (i.e. 2071-2100 minus present climate) is generally characterized with mixed increase and decrease in global solar radiation across the country than the previous two periods (1 and 2). For the annual potential future changes, RegCM3 model predicted a decrease in solar radiation towards the end of the century with more reduction found in the South zone and the least in the North region. Furthermore, future changes in global solar radiation across the zones in all the periods are however found to be insignificant at p <= 0.01. (c) 2015 Elsevier Ltd. All rights reserved.
机译:在这项研究中,使用国际理论物理中心(ICTP)1981年至2100年的区域气候模型第3版(RegCM3),以ECHAM5 GCM作为横向边界条件,模拟了尼日利亚在较高的大气CO2水平下的全球太阳辐射。使用NIMET和NASA观测数据集对RegCM3进行的模拟季节性全球太阳辐射偏差在控制期间的幅度相似,并显示出介于-10%到30%之间的持续正偏差和负偏差。该模型通常会在大多数月份中低估整个国家的太阳辐射(偏向-10%至-30%)。此外,它高估了该国北部地区的辐射(偏向+ 2-30%)。除了当前的气候(1981-2010年)之外,还考虑了三个未来时期:第一个时期(2011-2040年),第二个时期(2041-2070年)和第三个时期(2071-2100年),以应对潜在的未来变化。第1阶段的季节性潜在未来变化(即,相对于2040年的潜在未来变化)显示减少幅度为0%(北部)至3.27%(南部),而在第2阶段观察到全球太阳辐射的减少幅度更大(即, 2041-2070减去当前气候)总体下降幅度在0.11%至3.39%之间,其中4月份最低(中间带),南部地区最大(3月)。第3阶段(即2071-2100减去当前气候)未来的潜在变化通常以与前两个阶段(1和2)相比,全国范围内全球太阳辐射的增减混合为特征。对于未来的年度潜在变化,RegCM3模型预测到本世纪末太阳辐射将减少,南部地区的减少更多,而北部地区的减少最少。此外,发现在所有时期内,整个区域内日光辐射的未来变化在p <= 0.01时都是微不足道的。 (c)2015 Elsevier Ltd.保留所有权利。

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