Potential satellite mission on atmospheric dynamics for severe weather forecasts (Conference Presentation)

B. Lin, Q. Min, S. Harrah, Yongxiang Hu, R. Lawrence
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Abstract

Surface air pressure is the most important atmospheric variable for atmospheric dynamics. It is regularly measured by in-situ meteorological sensors, and there are no operational capabilities that could remotely sense the pressure over the globe. The poor spatiotemporal coverage of this dynamically crucial variable is a significant observational gap in weather predictions. To improve forecasts of severe weather conditions, especially the intensity and track of tropical storms, large spatial coverage and frequent sampling of surface barometry are critically needed for numerical weather forecast models. Recent development in remote sensing techniques provides a great hope of atmospheric barometry in large spatiotemporal scales. Currently, NASA Langley Research Center tries to use the concept of Differential-absorption Barometric Radar (DiBAR) working at the 50-56 GHz O2 absorption bands to fill the observational gap. The numerical simulation shows that with this DiBAR remote sensing system, the uncertainty in instantaneous radar surface air pressure estimates can be as low as ~1 mb. Prototype instrumentation and its related laboratory, ground and airborne experiments indicate that satellite DiBAR remote sensing systems will obtain needed air pressure observations and meet or exceed the science requirements for surface air pressure fields. Observational system simulation experiments (OSSEs) for space DiBAR performance based on the existing DiBAR technology and capability show substantial improvements in tropical storm predictions, not only for the typhoon track and position but also for the typhoon intensity. Satellite DiBAR measurements will provide an unprecedented level of the prediction and knowledge on global extreme weather conditions. A space multi-frequency differential oxygen absorption radar system will fill the gap in the global observations of atmospheric air pressure, increase our knowledge in the dynamics, and significantly improve weather, especially severe weather such as typhoon and hurricane, predictions. Advanced tropical storm forecasts are expected with the studied capability. The development of the DiBAR system and associated OSSE results will be presented.
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可能用于恶劣天气预报的大气动力学卫星任务(会议介绍)
地表气压是大气动力学中最重要的大气变量。它是由现场气象传感器定期测量的,目前还没有可以远程感知全球压力的操作能力。这一动态关键变量的低时空覆盖是天气预报中一个重要的观测缺口。为了改进对恶劣天气条件的预报,特别是对热带风暴的强度和路径的预报,数值天气预报模式迫切需要大的空间覆盖范围和频繁的地面气压采样。近年来遥感技术的发展为实现大时空尺度的大气气压测量带来了希望。目前,美国宇航局兰利研究中心试图使用差分吸收大气雷达(DiBAR)的概念,在50-56 GHz的O2吸收波段工作,以填补观测空白。数值模拟结果表明,利用该DiBAR遥感系统,雷达瞬时地面气压估计的不确定性可低至~1 mb。样机及其相关的实验室、地面和机载实验表明,卫星DiBAR遥感系统将获得所需的气压观测值,并满足或超过地面气压场的科学要求。基于现有DiBAR技术和能力对空间DiBAR性能进行的观测系统模拟实验(OSSEs)表明,无论是对台风路径和位置,还是对台风强度的预测,都有实质性的改进。卫星DiBAR测量将提供前所未有的全球极端天气条件预测和知识水平。空间多频差氧吸收雷达系统将填补全球大气气压观测的空白,增加我们在动力学方面的知识,并显著改善天气,特别是台风和飓风等恶劣天气的预测。利用所研究的能力,预期可作出较早的热带风暴预报。将介绍DiBAR系统的开发和相关的OSSE结果。
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