通过分析降水和边界层方案,改进水文气象耦合模拟中的飓风强度和流量预报

IF 3.1 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Md. Murad Hossain Khondaker, Mostafa Momen
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引用次数: 0

摘要

飓风是美国历史上破坏力最大、代价最高的水文气象事件,造成了灾难性的大风和洪水。飓风动力学会对风暴降水的数量和空间范围产生重大影响。然而,飓风强度与降水量之间复杂的相互作用,以及改善飓风动态对流量预测的影响尚未得到很好的证实。本文通过全面描述垂直扩散在不同行星边界层、微物理和积云参数化条件下对改善飓风强度和流场预报的作用,弥补了这些空白。为此,将天气和研究预测(WRF)大气模型与 WRF 水文模型(WRF-Hydro)相结合,模拟了在美国三个飓风多发地区登陆的四次主要飓风。首先,在 WRF-Hydro 中进行了逐步校准,与美国地质调查局(USGS)的水文站相比,该校准显著减少了水流预报误差。然后,进行了 60 次水文气象耦合模拟,以评估当前天气参数化的性能。结果表明,所有方案都低估了所观测到的主要飓风的强度,因为它们的扩散对飓风流模拟的影响过大。与默认模型相比,通过减少垂直扩散,飓风强度预报平均提高了约 39.5%。这些增强的飓风产生了更强的局地降水强迫。强度的增强使飓风流偏差和相关性预测分别提高了约 16% 和约 34%。这项研究强调了改进的飓风动力学在加强洪水预测中的作用,并为垂直扩散对飓风强度和流场预报的影响提供了新的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Improving hurricane intensity and streamflow forecasts in coupled hydro-meteorological simulations by analyzing precipitation and boundary layer schemes
Hurricanes have been the most destructive and expensive hydro-meteorological event in US history, causing catastrophic winds and floods. Hurricane dynamics can significantly impact the amount and spatial extent of storm precipitation. However, the complex interactions of hurricane intensity and precipitation and the impacts of improving hurricane dynamics on streamflow forecasts are not well established yet. This paper addresses these gaps by comprehensively characterizing the role of vertical diffusion in improving hurricane intensity and streamflow forecasts under different planetary boundary layer, microphysics, and cumulus parameterizations. To this end, the Weather and Research Forecasting (WRF) atmospheric model is coupled with the WRF hydrological model (WRF-Hydro) to simulate four major hurricanes landfalling in three hurricane-prone regions in the US. First, a stepwise calibration is carried out in WRF-Hydro, which remarkably reduces streamflow forecast errors compared to the United States Geological Survey (USGS) gauges. Then, 60 coupled hydro-meteorological simulations were conducted to evaluate the performance of current weather parameterizations. All schemes were shown to underestimate the observed intensity of the considered major hurricanes since their diffusion is over-dissipative for hurricane flow simulations. By reducing the vertical diffusion, hurricane intensity forecasts were improved by ~39.5% on average compared to the default models. These intensified hurricanes generated more intense and localized precipitation forcing. This enhancement in intensity led to ~16% and ~34% improvements in hurricane streamflow bias and correlation forecasts, respectively. The research underscores the role of improved hurricane dynamics in enhancing flood predictions and provides new insights into the impacts of vertical diffusion on hurricane intensity and streamflow forecasts.
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来源期刊
Journal of Hydrometeorology
Journal of Hydrometeorology 地学-气象与大气科学
CiteScore
7.40
自引率
5.30%
发文量
116
审稿时长
4-8 weeks
期刊介绍: The Journal of Hydrometeorology (JHM) (ISSN: 1525-755X; eISSN: 1525-7541) publishes research on modeling, observing, and forecasting processes related to fluxes and storage of water and energy, including interactions with the boundary layer and lower atmosphere, and processes related to precipitation, radiation, and other meteorological inputs.
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