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Simulated Hydrologic Responses to Climate Variations and Change in the Merced, Carson, and American River Basins, Sierra Nevada, California, 1900–2099

机译:1900年至2099年,加利福尼亚内华达州默塞德河,卡森河和美国流域对气候变化和变化的模拟水文响应

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摘要

Hydrologic responses of river basins in the Sierra Nevada of California to historical and future climate variations and changes are assessed by simulating daily streamflow and water-balance responses to simulated climate variations over a continuous 200-yr period. The coupled atmosphere-ocean-ice-land Parallel Climate Model provides the simulated climate histories, and existing hydrologic models of the Merced, Carson, and American Rivers are used to simulate the basin responses. The historical simulations yield stationary climate and hydrologic variations through the first part of the 20th century until about 1975 when temperatures begin to warm noticeably and when snowmelt and streamflow peaks begin to occur progressively earlier within the seasonal cycle. A future climate simulated with business-as-usual increases in greenhouse-gas and aerosol radiative forcings continues those recent trends through the 21st century with an attendant +2.5 °C warming and a hastening of snowmelt and streamflow within the seasonal cycle by almost a month. The various projected trends in the business-as-usual simulations become readily visible despite realistic simulated natural climatic and hydrologic variability by about 2025. In contrast to these changes that are mostly associated with streamflow timing, long-term average totals of streamflow and other hydrologic fluxes remain similar to the historical mean in all three simulations. A control simulation in which radiative forcings are held constant at 1995 levels for the 50 years following 1995 yields climate and streamflow timing conditions much like the 1980s and 1990s throughout its duration. The availability of continuous climate-change projection outputs and careful design of initial conditions and control experiments, like those utilized here, promise to improve the quality and usability of future climate-change impact assessments.
机译:加利福尼亚内华达山脉河流域对历史和未来气候变化和变化的水文响应通过模拟连续200年的模拟气候变化的日流量和水平衡响应来评估。大气-海-冰-土地耦合的并行气候模型提供了模拟的气候历史,并使用了默塞德河,卡森河和美国河流的现有水文模型来模拟流域响应。历史模拟产生了整个20世纪上半叶直到1975年左右的固定气候和水文变化,当时温度开始明显变暖,而融雪和水流高峰在季节周期的早期开始逐渐出现。通过像往常一样的温室气体和气溶胶辐射强迫的增加来模拟未来的气候,延续了21世纪的最新趋势,伴随着+2.5°C的变暖以及季节性周期内将融雪和水流加速了将近一个月。 。尽管可以在2025年左右模拟出自然的自然气候和水文变化,但仍可以照常观察到通常的模拟中的各种预计趋势。与这些变化主要相关的是水流时间,长期平均水流和其他水文状况在所有三个模拟中,通量都保持与历史平均值相似。在1995年之后的50年中,将辐射强迫保持在1995年水平不变的控制模拟会产生气候和水流定时条件,就像整个时期的1980年代和1990年代一样。像这里使用的那样,可获得连续的气候变化预测输出以及精心设计的初始条件和控制实验,有望提高未来气候变化影响评估的质量和可用性。

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  • 来源
    《Climatic Change》 |2004年第3期|283-317|共35页
  • 作者单位

    Scripps Institution of Oceanography Dept. 0224 U.S. Geological Survey;

    Scripps Institution of Oceanography Dept. 0224 U.S. Geological SurveyClimate Research Division Scripps Institution of Oceanography University of California;

    Climate Research Division Scripps Institution of Oceanography University of California;

    U.S. Geological Survey;

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  • 正文语种 eng
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  • 入库时间 2022-08-18 02:12:46

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