首页> 外文期刊>Global and planetary change >Multi-model ensemble projections in temperature and precipitation extremes of the Tibetan Plateau in the 21st century
【24h】

Multi-model ensemble projections in temperature and precipitation extremes of the Tibetan Plateau in the 21st century

机译:21世纪青藏高原极端温度和降水的多模式集合投影

获取原文
获取原文并翻译 | 示例
           

摘要

Projections of changes in climate extreme are important in assessing the potential impacts of climate change on social and natural systems. This article presents future projections of climate extremes in the Tibetan Plateau constructed from ensembles of coupled general circulation models (CGCMs) contributing to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC AR4), under a range of emission scenarios. The extremes of temperature and precipitation are described by seven indices, namely, the frost day (FD), percentage of nights when T_(min)>90th percentile (TN90), consecutive dry days (CDD), annual count of days when precipitation >=10 mm (RIO), maximum 5-day precipitation total (R5D), simple daily intensity index (SDH), and annual total precipitation when precipitation >95th percentile (R95T). Results indicate that frost days decrease over the Tibetan Plateau in the 21st century. More frequent warm nights are also projected in the plateau. The increases of these temperature extremes under A2 and A1B scenarios are more pronounced than under Bl. Heavy precipitation events for single days and pentads are projected to increase in their intensity over most parts of Tibetan Plateau. CDD, RIO, R5D, R95T and SDII collectively suggest more extreme precipitation in the region (2011-2020). In addition, impacts of climate extremes changes on local water resources and fragile ecosystem are discussed as an extension of this article. The findings will be beneficial to project regional responses in this unique region to global climate change, and then to formulate regional strategies against the potential menaces of climate change.
机译:气候极端变化的预测对于评估气候变化对社会和自然系统的潜在影响至关重要。本文介绍了在一系列排放情景下,由对政府间气候变化专门委员会第四次评估报告(IPCC AR4)做出贡献的耦合的一般环流模型(CGCM)构成的青藏高原的极端气候预测。温度和降水的极端值由七个指标来描述,即霜冻日(FD),T_(min)> 90%百分数(TN90)时的夜晚百分比,连续干旱天(CDD),降水> = 10毫米(RIO),最大5天降水总量(R5D),简单日强度指数(SDH),以及当降水> 95%时年降水量(R95T)。结果表明,在21世纪,青藏高原的霜冻日减少。高原地区还将出现更频繁的暖夜。在A2和A1B情景下,这些极端温度的升高比在B1下更为明显。在青藏高原的大部分地区,单日和五元组的强降水事件预计会增加强度。 CDD,RIO,R5D,R95T和SDII共同表明该地区出现了更多极端降雨(2011-2020年)。此外,本文还扩展了极端气候变化对当地水资源和脆弱生态系统的影响。这些发现将有助于在这个独特的地区对全球气候变化做出区域反应,然后针对气候变化的潜在威胁制定区域战略。

著录项

  • 来源
    《Global and planetary change》 |2012年第1期|p.1-13|共13页
  • 作者单位

    State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, China ,State Key Laboratory of Hydrology-Water Resources and Hydraulics Engineering, Hohai University, Nanjing 210098, China;

    State Key Laboratory of Hydrology-Water Resources and Hydraulics Engineering, Hohai University, Nanjing 210098, China;

    CSIRO Mathematics, Informatics and Statistics, Private Bag 5, Wembley, WA 6913, Australia;

    Department of Geosciences, University of Oslo, P.O. Box 1047, Blindern, 0316 Oslo, Norway;

    State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, China;

    State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, China;

    State Key Laboratory of Hydrology-Water Resources and Hydraulics Engineering, Hohai University, Nanjing 210098, China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    climate extremes; indices; multi-model ensemble; projection; scenarios; bayesian model averaging (BMA); the tibetan plateau;

    机译:气候极端事件;指标;多模型合奏;投影;情景;贝叶斯平均模型(BMA);西藏高原;

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号