Use of Doppler Radar Winds in a Non-Convective Event
收藏NOAA Institutional Repository2025-05-23 更新2026-04-25 收录
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In this weather event, Doppler radar winds provided a frequent upper-wind profile that filled the gap between 12-hourly RAOBs. Although surface winds were also backing prior to the changeover to snow, knowledge of the change in the upper-level winds provided evidence that this was not just a local aberration in the wind field.
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NOAA
创建时间:
2025-05-23



