首页> 外文期刊>Water News A propos de l'eau >Modelling historical and potential future climate impacts on Keremeos Creek, an Okanagan-Similkameen watershed, British Columbia, Canada: Part Ⅰ. Forecasting change in spring and summer water supply and demand
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Modelling historical and potential future climate impacts on Keremeos Creek, an Okanagan-Similkameen watershed, British Columbia, Canada: Part Ⅰ. Forecasting change in spring and summer water supply and demand

机译:对加拿大不列颠哥伦比亚省Okanagan-Similkameen流域Keremeos Creek的历史和潜在未来气候影响进行建模:第一部分。

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The current study is Part I of a two-part assessment of climate change impacts on hydrology and farm-level Greenhouse Gas (GHG) emissions. The effects of climate change on spring and summer water supply and spring and summer water demand related to the vegetation cover in the Keremeos Creek watershed in the Regional District of Okanagan-Similkameen (RDOS), southern British Columbia, Canada in the time-frame of 1961 to 2100 are investigated in Part I. The GENerate Earth SYstems Science input (GENESYS) spatial hydro-meteorological model is applied to predict the potential changes for the ensemble averages of 15 General Circulation Models (GCMs) for two Representative Concentration Pathways (RCP) scenarios (RCP 4.5 and RCP 8.5) in the 2020's (2011-2040), 2050's (2041-2070), and 2080's (2071-2100) relative to the 1961-1990 base period. Timing of snowmelt may be expected to occur one month earlier in all projected periods with RCP 4.5 and 8.5 except RCP 8.5 in the 2080's, which may be 2 months earlier relative to the 1961-1990 period. Based on predictions, there may be increases in total spring water supply from 35% to 39% and decreases in summer water supply from 36% to 79% relative to the 1961-1990, based on the three projected periods with RCP 4.5 and 8.5. Average spring vegetation water demand may increase from 20% to 47% but summer vegetation water demand may decrease from 10% to 29% relative to the 1961-1990 period based on the projected periods and emission scenarios. The spring and summer evapotranspiration estimates were controlled by the surface energy and soil moisture availability, respectively. These changes are expected to put stress on the future water resources management in the watershed. The results of Part I are then applied to Part II to estimate changes in farm-level GHG emissions and soil carbon storage.
机译:当前的研究是气候变化对水文和农场一级温室气体(GHG)排放的影响的两部分评估的第一部分。气候变化对春季和夏季供水和春季和夏季需水量的影响与加拿大不列颠哥伦比亚省南部的欧肯娜根-西米尔卡梅恩(RDOS)区域地区的Keremeos Creek流域的植被覆盖有关,时间间隔为在第一部分中研究了1961年至2100年。广义地球系统科学输入(GENESYS)空间水文气象模型被用于预测两个代表性浓度路径(RCP)的15个一般环流模型(GCM)集合平均值的潜在变化。相对于1961-1990年基期的2020年(2011-2040年),2050年(2041-2070年)和2080年(2071-2100年)情景(RCP 4.5和RCP 8.5)。在RCP 4.5和8.5的所有预计时期中,预计融雪的时间会提前一个月,而2080年代的RCP 8.5除外,相对于1961-1990年可能要早两个月。根据预测,基于RCP 4.5和8.5的三个预测时期,相对于1961-1990年,春季总供水量将从35%增加到39%,夏季供水量将从36%减少到79%。根据预计的时期和排放情景,相对于1961-1990年,春季植被的平均需水量可能会从20%增至47%,但夏季植被的需水量可能会从10%降至29%。春季和夏季的蒸散量估计分别由表面能和土壤水分的可利用性控制。这些变化有望给流域未来的水资源管理带来压力。然后,将第一部分的结果应用于第二部分,以估算农场一级温室气体排放量和土壤碳储量的变化。

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