Method to estimate intensity of tropical cyclone across the Northwest Pacific Ocean by using geostationary meteorological satellite image
A geostationary meteorological satellite, tropical cyclone technology, applied in the field of atmospheric scientific research, can solve the problems of cirrus cloud interference and divergence in the IRW cloud image of the geostationary meteorological satellite
Patent Information
- Authority / Receiving Office
- CN · China
- Current Assignee / Owner
- Publication Date
- 2014-09-10
- Estimated Expiration
- Not applicable · inactive patent
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Abstract
Description
technical field
[0001] The invention relates to a method for estimating the intensity of a tropical cyclone, in particular to a method for estimating the intensity of a tropical cyclone by using static meteorological satellite images, and belongs to the field of atmospheric science research. Background technique
[0002] Typhoons are the most serious natural disasters, and both coastal areas and inland areas hundreds of kilometers away from the sea may be affected by them. Real-time monitoring of the birth, development and strengthening of typhoons can ensure timely emergency response and effectively reduce local economic losses and casualties. Geostationary meteorological satellite remote sensing has high time resolution (compared to microwave remote sensing of polar-orbiting satellites, such as Velden et al. 1992; Wu et al.2005; Aberson et al.2006), the advantages of being able to cover oceans and sparsely populated areas (compared to ground-based radars such as Corbosier...
Examples
Embodiment Construction
[0036] The scheme of the present invention is described in detail below:
[0037] The first step is preprocessing:
[0038] We selected all 35 strong typhoon cases from 2006 to 2011, and the detailed information is shown in Table 2:
[0039] Table 2. Names and IDs of 35 strong typhoon cases.
[0040]
[0041] The brightness temperature information of the infrared window area and the water vapor channel of the typhoon core area is extracted from the satellite cloud images of equal latitude and longitude at various times corresponding to the typhoon. The core area refers to the area within 150km from the center of the typhoon.
[0042] The second step is to confirm the WIRa parameters:
[0043] This parameter can distinguish common convection from cirrus, penetrating convection, and water vapor anomalies on static satellite cloud images. Its theoretical basis is as follows: As shown in Table 3, the negative Tb WV-IRW is caused by cirrus clouds and weak convection, and the...