摘要
区域蒸散量(evapotranspiration)预测对精准灌溉预报与农田水分管理意义重大。该文利用川中丘陵区11个气象站点1961-2013年逐日气象资料,采用FAO-56 Penman-Monteith公式计算参考作物蒸散量(reference evapotranspiration,ET0),基于Hadley Centre Coupled Model version 3(HadCM3)的输出和统计降尺度模型(statistical downscaling model,SDSM)分别对A2(高温室气体排放)、B2(低温室气体排放)情景下川中丘陵区2014-2099年ET0进行预测,并使用Mann-Kendall检验和反距离加权插值法对1961-2099年ET0的时空演变特征进行分析。结果表明:基准期(1961-2010年)川中丘陵区ET0整体呈现明显下降趋势,空间上呈现出东北部、西北部和东南部相对较大、中部相对较小的差异;与基准期相比,A2、B2情景下未来2020 s(2011-2040年)、2050 s(2041-2070年)和2080 s(2071-2099年)川中丘陵区ET_0月和年均值都呈增大趋势;A2情景下3个时期ET0将分别增加7.9%、10.9%和16.7%,B2情景下ET_0将分别增加7.1%、4.9%和12.8%;A2、B2情景下3个时期川中丘陵区ET_0空间分布均呈现西北部和南部较大、中部较小的空间差异,且3个时期的ET0相对变化率显示中部及其偏北、偏南区域ET_0增幅相对较大,北部和南部增幅相对较小。因此,未来川中丘陵区ET0的上升可能导致水资源短缺与季节性干旱进一步加剧。该研究可为川中丘陵区水资源优化管理和灌溉制度制定提供科学参考。
Reference evapotranspiration(ET0) is an important component of agricultural water management, analysis on the change trend and spatial distribution characteristics of ET0 under the climate change scenarios can be used as references for estimation of crop water requirement. In the current study, daily meteorological data from 11 meteorological stations were obtained from 1961 to 2013 in hilly area of central Sichuan, Southwest China. ET0 during 1961-2013 were calculated by FAO-56 Penman-Monteith equation, ET0 during 2014-2099 were downscaled from Had CM3(Hadley Centre Coupled Model version 3) outputs under two emission scenarios of high(A2) and low(B2) emission by statistical downscaling model(SDSM 4.2 software). Temporal trend and spatial distribution of ET0 during 1961-2099 were analyzed by Mann-Kendall trend test and Inverse Distance Weighted Interpolation method. The results indicated that ET0 decreased non-significantly(P>0.05) during baseline period(1961-2010) with a tendency rate of-5.2 mm/10 a, annual mean ET0 was 757 mm, and the highest values of ET0 were found in the north and south region while the lowest values were in the central region; Had CM3 projected a statistically significant(P<0.05) and continuous increase in ET0 during 2020s(2011-2040), 2050s(2041-2050) and 2080s(2071-2099) with a rate of 8.9, 17.5 and 13.2 mm/10 a under A2 emission scenario and 12.1, 21.5 and 4.3 mm/10 a under B2 emission scenario, respectively. Averaged for the whole area, the projected increase were 7.9%, 10.9% and 16.7% under A2 emission scenario and 7.1%, 4.9% and 12.8% under B2 emission scenario for the three periods 2020 s, 2050 s and 2080 s, respectively. The increase under A2 emission scenario was slightly higher than that under B2 scenario which may be caused by higher air temperature and solar radiation under A2 emission scenario. The highest values of ET0 were found in the northwest and south region while the lowest values were in the central region both under A2 and B2 emission scenarios for the three periods 2020 s, 2050 s and 2080 s, and the greater increase in ET0 was found in south central region while lower increase was in central, south and north region both under A2 and B2 emission scenarios for the three periods 2020 s, 2050 s and 2080 s. GCMs and SDSM were applied to project the climate changes in the future, which may lead some uncertainties in the results due to the uncertainties of GCMs, SDSMs and selection of predictors. In order to reduce the uncertainties of climate projection and improve the simulating abilities of SDSMs on future climate, more GCMs, downscaling methods and emission scenarios should be selected for the projection of ET0. This research provided possible temporal trend and spatial distribution of ET0 in the future in hilly area of central Sichuan, which can provide valuable information for irrigation schedule planning.
出处
《农业工程学报》
EI
CAS
CSCD
北大核心
2016年第S1期71-79,共9页
Transactions of the Chinese Society of Agricultural Engineering
基金
国家科技支撑计划项目(2015BAD24B01)
农业部旱作节水农业重点实验室基金(HZJSNY201502)
四川省软科学研究计划项目(2015ZR0157)
国家自然科学基金(51009101)
南方丘区节水农业研究四川省重点实验室开放基金(JSSYS2014-C)
关键词
气候变化
蒸散
模型
预测
HadCM3
统计降尺度
气候情景
川中丘陵区
climate change
evapotranspiration
models
projection
Had CM3
statistical downscaling model
climate scenario
hilly area of central Sichuan
