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Analysis and prediction of dryland land-surface processes and their influence on the meteorology of the Intermountain West.

机译:旱地地表过程的分析和预测及其对西部山间气象的影响。

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摘要

This dissertation examines the performance of Weather Research and Forecasting (WRF) model near-surface temperature and surface energy balance forecasts over Dugway Proving Ground (DPG) in northwest Utah during the Mountain Terrain Atmospheric Modeling and Observations Program (MATERHORN) field campaigns. This region of complex terrain has two distinct land surfaces, playa and sparsely vegetated desert shrub, which are common in other dryland regions. Operational WRF forecasts show persistent underprediction of the diurnal temperature range due to a nighttime warm bias and a daytime cold bias. The former is especially strong over the desert shrub. The nighttime warm bias can be improved through the utilization of in situ soil moisture observations and by replacing Johansen's 1975 parameterization of soil thermal conductivity in the Noah land surface model with that proposed by McCumber and Pielke in 1981 for silt loam and sandy loam soils.;The daytime cold bias extends from the surface to above the top of the planetary boundary layer and is primarily caused by a regional overestimation of near-surface soil-moisture in operational land-surface analyses, which do not currently assimilate in situ soil-moisture observations. Bias correction of the soil-moisture analyses across the Intermountain West using North American Soil Moisture Database observations reduces the daytime cold bias.;Utilization of observed soil moisture and the McCumber and Pielke soil thermal conductivity parameterization also improves the surface energy balance forecast over the desert shrub, but degrades it over the playa. Land surface processes unique to the playa are not currently accounted for in the Noah land surface model. Nevertheless, a larger and more accurate temperature gradient develops between the playa and desert shrub that forces a stronger daytime off-playa breeze. However, 10-m wind speed and direction forecasts show limited statistically significant improvement.;This dissertation also presents a climatology of episodic dust events across the Intermountain West and locates dust source regions through a dust retrieval algorithm adapted for data from geostationary operational environmental satellites.
机译:本文研究了在犹他州西北部山区地形大气建模与观测计划(MATERHORN)野外活动期间,气象研究与预测(WRF)模型近地面温度和地面能量平衡预测在犹他州西北部Dugway试验场(DPG)上的性能。这个地形复杂的地区有两个截然不同的陆地表面,即普拉亚和稀疏的沙漠灌木丛,这在其他旱地地区很常见。 WRF的运行预测表明,由于夜间的暖偏和白天的冷偏,对昼夜温度范围的持续低估。前者在沙漠灌木丛上特别强。通过利用原位土壤水分的观测值和用约翰·麦克森和皮尔克在1981年提出的针对淤泥壤土和沙质壤土的方法代替Johansen于1975年在Noah地表模型中对土壤热导率的参数化,可以改善夜间的热偏差。白天的冷偏差从地表延伸到行星边界层的顶部以上,主要是由于在可操作的地表分析中对近地表土壤水分的区域高估所致,目前尚无法同化原地的土壤水分观测结果。 。使用北美土壤水分数据库的观测结果对整个山间西部的土壤水分分析进行偏差校正可减少白天的冷偏差。利用观测到的土壤水分以及McCumber和Pielke的土壤热导率参数化还可以改善沙漠表面的地表能量平衡预测灌木丛,但会在海滩上使之退化。诺亚(Noah)地表模型目前未考虑普拉亚特有的地表过程。但是,在普拉亚和沙漠灌木之间会形成一个更大,更准确的温度梯度,从而迫使白天的非普拉亚微风更加强烈。然而,10米的风速和风向预报在统计学上没有显着的改善。;本论文还介绍了整个西山间的偶发性尘埃事件的气候学,并通过适用于对地静止运行环境卫星数据的尘埃检索算法确定了尘埃源区域。

著录项

  • 作者

    Massey, Jeffrey Duffus.;

  • 作者单位

    The University of Utah.;

  • 授予单位 The University of Utah.;
  • 学科 Atmospheric sciences.
  • 学位 Ph.D.
  • 年度 2015
  • 页码 230 p.
  • 总页数 230
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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