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Of warming nights and shifting winds.

机译:温暖的夜晚和多风的天气。

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摘要

The attribution of recent global warming to anthropogenic emissions is now well established. However, the relation of recent changes in other properties of the climate system to human activities is not as clearly understood. The aim of this thesis is to improve our understanding of this relation in the case of two of these properties, namely the diurnal temperature range (DTR) and modes of tropospheric variability.; The DTR, the difference between daily maximum and minimum temperatures, has decreased over global land areas at a rate comparable to the mean warming. Model simulations including the effects of human emissions produce a comparable change, albeit of smaller magnitude. This decrease results from increased reflection of solar radiation by clouds moderated by decreasing soil moisture, mostly through its effect on the ground heat capacity.; Recent trends in indices of some modes of atmospheric variability suggest the possibility that forced climate change may manifest itself through a projection onto these pre-existing modes. Model simulations indicate that this is plausible in the case of sea level pressure, but only partly so in the case of surface air temperature. On the interannual time scale examined in this thesis, these projections are consistent with a linear interpretation, rather than a nonlinear one.; These results are, however, sensitive to the representation of small scale processes in the models. For instance, the DTR response depends strongly on the representation of cloud and land surface processes. Further examination of the response of one of the tropospheric modes, namely the Southern Annular Mode which represents the meridional shift of the mid latitude jet in the Southern Hemisphere, indicates that it is sensitive to the parametrisation of sub-grid scale mixing in the ocean. Nevertheless, these results suggest that the recent changes are consistent with enhanced greenhouse warming, and indicate that they are likely to continue into the foreseeable future.
机译:现在已经确定了近期全球变暖与人为排放的关系。然而,人们对气候系统其他特性的最新变化与人类活动之间的关系的了解还不清楚。本文的目的是在其中两个特性(即昼夜温度范围(DTR)和对流层变率模式)的情况下增进我们对这种关系的理解。 DTR是每日最高和最低温度之间的差异,在全球陆地面积上以与平均变暖相当的速度下降。包括人类排放物影响在内的模型模拟会产生可比较的变化,尽管幅度较小。减少的原因是由于土壤水分减少(主要是由于其对地热容量的影响)而减弱的云对太阳辐射的反射增加。某些大气变率模式指数的最新趋势表明,强迫气候变化可能会通过对这些既有模式的预测而显现出来。模型仿真表明,在海平面压力的情况下,这是合理的,但在地表空气温度的情况下,这仅是部分原因。在本文研究的年际时间尺度上,这些预测与线性解释一致,而不是非线性解释。但是,这些结果对模型中小规模过程的表示很敏感。例如,DTR响应在很大程度上取决于云和陆地表面过程的表示。进一步检查对流层模式之一的响应,即表示南半球中纬度射流经向位移的南环形模式,表明它对海洋中次网格尺度混合的参数化很敏感。然而,这些结果表明,最近的变化与温室效应的加剧是一致的,并且表明它们可能会持续到可预见的未来。

著录项

  • 作者

    Stone, Daithi Alastar.;

  • 作者单位

    University of Victoria (Canada).;

  • 授予单位 University of Victoria (Canada).;
  • 学科 Physical Oceanography.; Environmental Sciences.
  • 学位 Ph.D.
  • 年度 2003
  • 页码 103 p.
  • 总页数 103
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 海洋物理学;环境科学基础理论;
  • 关键词

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