The impacts of assimilating Aeolus horizontal line-of-sight winds on numerical predictions of Hurricane Ida (2021) and a mesoscale convective system over the Atlantic Ocean
The Aeolus satellite, the first spaceborne wind lidar launched by the European Space Agency (ESA) on 22 August 2018, provides global measurements of horizontal line-of-sight (HLOS) winds. The assimilation of Aeolus HLOS winds has been proven to improve numerical weather predictions (NWPs). Still, it...
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Veröffentlicht in: | Atmospheric measurement techniques 2023-06, Vol.16 (10), p.2691-2708 |
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Zusammenfassung: | The Aeolus satellite, the first spaceborne wind lidar
launched by the European Space Agency (ESA) on 22 August 2018, provides
global measurements of horizontal line-of-sight (HLOS) winds. The
assimilation of Aeolus HLOS winds has been proven to improve numerical
weather predictions (NWPs). Still, its influences on forecasts of tropical
cyclones (TCs) and tropical convective systems have yet to be examined in
detail. This study investigates the impacts of assimilating Aeolus HLOS
winds on the analysis and forecasts of Hurricane Ida (2021) and a mesoscale
convective system (MCS) embedded in an African easterly wave (AEW) over the
Atlantic Ocean (AO) with the mesoscale community Weather Research and
Forecasting (WRF) model and the NCEP Gridpoint
Statistical Interpolation (GSI)-based three-dimensional
ensemble-variational (3DEnVAR) hybrid data assimilation (DA) system.
Mie-cloudy and Rayleigh-clear winds are assimilated. The results for Ida
(2021) show that assimilating Aeolus HLOS winds leads to better track
predictions. The intensity forecasts are improved in some cases, even with
limited coverage of Aeolus HLOS winds within the inner core region of Ida
(2021). In addition, the structure of heavy precipitation associated with
Ida (2021) is refined after the assimilation of Aeolus HLOS winds. Further
diagnosis demonstrates that the improved intensity and precipitation
forecasts result from enhanced divergence in the upper level of the
troposphere after the assimilation of Aeolus HLOS winds. Additional results from
the MCS associated with an AEW indicate that assimilating Aeolus HLOS winds
enhances forecasts of its precipitation structure and the associated
low-level divergence. Findings from this study suggest that the assimilation of
Aeolus HLOS winds has the potential to improve forecasts for TCs and
tropical convective systems. |
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ISSN: | 1867-8548 1867-1381 1867-8548 |
DOI: | 10.5194/amt-16-2691-2023 |