GB/T 36745-2018 in English
VALIDSpecification for typhoon cyclone observational wind data differentiating
- Issued on:2018-09-17
- Implemented on:2019-04-01
- File Format:PDF
- Delivery:Via email within 1~3 business days
$156.00
《GB/T 36745-2018台风涡旋测风数据判别规范》由TC345(全国气象防灾减灾标准化技术委员会)归口,主管部门为中国气象局。
Introduction
In-depth interpretation of the typhoon vortex wind measurement data identification specification
1. Background and significance of standard formulation
GB/T 36745-2018 "Typhoon vortex wind measurement data identification specification" is an important standard formulated to meet the needs of meteorological disaster prevention and mitigation and improve the level of typhoon monitoring technology. This standard is managed by the National Meteorological Disaster Prevention and Mitigation Standardization Technical Committee and drafted by the Public Meteorological Service Center of the China Meteorological Administration.
2. Comparison of standard frameworks
| Standard dimensions | Eye area characteristics | Eye wall strong wind area characteristics | Outer strong wind area characteristics |
|---|---|---|---|
| Average wind speed (m/s) | <=10 | >=17.2 | >=17.2 |
| Wind attack angle characteristics | Negative value | Positive value | No fixed pattern |
| Turbulence intensity | Low | High | Medium |
3. Technical Details of the Standard
3.1 Zoning Indicators of Typhoon Vortex
Based on the circulation structure characteristics of the typhoon vortex, this standard divides the typhoon wind conditions into three areas:
- Eye area: The central light wind area, with an average wind speed of less than or equal to 10 m/s.
- Eye wall strong wind area: The irregular annular strong wind belt surrounding the eye area, with the maximum wind speed and significantly increased turbulence parameters.
- Outer strong wind area: Characterized by an average wind speed of greater than or equal to 17.2 m/s, including the wind speed change area before and after the typhoon center passes.
3.2 Representativeness of wind data zoning
The representativeness of wind data zoning is determined based on the following indicators:
- Average wind speed is greater than or equal to 17.2 m/s: Wind direction changes continuously by more than 120 degrees in azimuth.
- Typhoon process wind speed time curve: Bimodal distribution or unimodal distribution.
- Bottom average wind speed between the two peaks: Less than or equal to 10 m/s.
4. Implementation suggestions and precautions
4.1 Data collection and processing
In actual applications, the collection and processing of wind data should be carried out in strict accordance with the standard requirements:
- Ensure that the time resolution of wind speed data is not less than once every 3 seconds.
- Use the calculation formula (A.1) of
average wind speed and the calculation formula (A.4) ofgust coefficient to verify the data.
4.2 Application scenarios and limitations
Although this standard provides a detailed identification method, it is still necessary to pay attention to the following in actual application:
- For typhoon monitoring stations under complex terrain conditions, it may be necessary to make adjustments in combination with the surface roughness and wind profile characteristics.
- It is recommended to combine
turbulence intensity andwind profile index for comprehensive identification during data analysis.
5. Practical Application Case Analysis
Take the 2018 No. 1 typhoon as an example. In the observation data of a coastal meteorological station, it is found that its wind speed time history curve presents a typical bimodal distribution feature. By calculating the

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