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首页> 外文期刊>Journal of great lakes research >Forecasting impacts of climate change on Great Lakes surface water temperatures
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Forecasting impacts of climate change on Great Lakes surface water temperatures

机译:预测气候变化对大湖地表水温的影响

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摘要

Temperature influences the rates of many ecosystem processes. A number ot recent studies have found evidence of systematic increases in Great Lakes surface water temperatures. Our study aims to construct empirical relationships between surface water temperatures and local air temperatures that can be used to estimate future water temperatures using future air temperatures generated by global climate models. Remotely sensed data were used to model lake-wide average surface water temperature patterns during the open-water period in Lakes Superior, Huron, Erie, and Ontario. Surface water temperatures typically exhibit linear warming through the spring, form a plateau in mid-summer and then exhibit linear cooling in fall. Lake-specific warming and cooling rates vary little from year to year while plateau values vary substantially across years. These findings were used to construct a set of lake-specific empirical models linking surface water temperatures to local air temperatures for the period 1995-2006. Hindcasted whole-lake water temperatures from these models compare favourably to independently collected offshore water temperatures for the period 1968-2002. Relationships linking offshore water temperatures to inshore water temperatures at specific sites are also described. Predictions of future climates generated by the Canadian Global Climate Model Version 2 (CGCM2) under two future greenhouse gas emission scenarios are used to scope future Great Lakes surface water temperatures: substantial increases are expected, along with increases in the duration of summer stratification.
机译:温度影响许多生态系统过程的速率。最近的许多研究已经发现大湖地表水温度系统升高的证据。我们的研究旨在构建地表水温度与当地气温之间的经验关系,这些关系可用于使用全球气候模型生成的未来气温来估算未来水温。在苏必利尔湖,休伦湖,伊利湖和安大略省的开阔水域,使用遥感数据对全湖平均地表水温模式进行建模。地表水温度通常在整个春季呈现线性变暖,在仲夏形成平稳期,然后在秋季呈现线性降温。每年因湖泊而异的增温和降温速率变化不大,而高原值则逐年变化很大。这些发现被用于构建一套针对湖的经验模型,将1995-2006年间的地表水温度与当地空气温度联系起来。这些模型的后预报全湖水温优于1968-2002年期间独立收集的近海水温。还描述了在特定地点将近海水温与近海水温联系起来的关系。加拿大全球气候模型第2版(CGCM2)在两种未来温室气体排放情景下产生的未来气候的预测被用于确定未来大湖的地表水温度:预计将有实质性的增加,以及夏季分层持续时间的增加。

著录项

  • 来源
    《Journal of great lakes research》 |2009年第3期|454-463|共10页
  • 作者单位

    Department of Ecology and Evolutionary Biology, University of Toronto, Canada, ON M5S 3B2 Harkness Laboratory of Fisheries Research, Aquatic Research and Development Section, Ontario Ministry of Natural Resources, 300 Water St., Peterborough, Canada, ON K9J 8M5;

    Department of Ecology and Evolutionary Biology, University of Toronto, Canada, ON M5S 3B2 Harkness Laboratory of Fisheries Research, Aquatic Research and Development Section, Ontario Ministry of Natural Resources, 300 Water St., Peterborough, Canada, ON K9J 8M5;

    Department of Ecology and Evolutionary Biology, University of Toronto, Canada, ON M5S 3B2 Great Lakes Laboratory for Fisheries and Aquatic Science, Fisheries and Oceans Canada, TO Box 5050. 867 Lakeshore Road, Burlington, Canada, ON L7R 4A6;

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

    climate change; surface water temperatures; great lakes;

    机译:气候变化;地表水温;五大湖;

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