The overlooked role of westerly moisture as a source of summer rainfall in the hyperarid Atacama Desert

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Title:Main Title: The overlooked role of westerly moisture as a source of summer rainfall in the hyperarid Atacama Desert
Description:Abstract: The Atacama receives significantly less precipitation than other deserts such as the Namib and Sahara. The persistent absence of water preserves the record of environmental change (e.g., precipitation characteristics), making it an invaluable proxy for studying the evolution of life on Earth. Due to the scarcity of in-situ measurements and difficulties in satellite remote sensing, information on precipitation characteristics is limited even for the present climate. Therefore, there are gaps in our understanding, especially for summer precipitation. During this season, moisture transport offshore Atacama’s coast could potentially trigger rainfall inland. To test this hypothesis, we identified 96 summer (November-March) rainfall events in the period 1961-2020 using 4 rain gauge stations and classified the synoptic conditions according to their similarities in circulation and moisture transport using the ERA5 reanalysis. The majority of rainfall episodes (83%) are associated with a stronger than normal and southward displaced Bolivian High in the upper troposphere and an anomalous 850 hPa low-pressure system off the coast of Atacama. The cyclonic circulation triggers moist northerlies along the southeastern Pacific in an elongated structure. Through composite analysis and a detailed case study (January 2019) using regional-scale high-resolution weather simulations (WRF), ground-based remote sensing at Iquique, and weather stations, we investigated the local circulation associated with these rain events. Daytime heating of the western slope of the Andes results in moisture transport inland. Topographically induced uplift leads to cloud formation and precipitation in the eastern Atacama. Moisture from the Pacific can even reach the western Altiplano, suggesting that the effect is not limited to the desert. A nocturnal return flux at ~3 km above sea level feeds moisture, clouds, and causes rainfall in the coastal region. To further investigate how this rainfall mechanism has changed in the current climate, we performed a trend analysis of circulation and water vapor using ERA5. Potential links with climate change (such as Hadley cell expansion) and impact on precipitation are also explored.
Responsible Party
Creators:José Vicencio Veloso (Author), Christoph Böhm (Author), Jan Schween (Author), Ulrich Löhnert (Author), Susanne Crewell (Author)
Publisher:CRC1211 Database (CRC1211DB)
Publication Year:2023
Topic
CRC1211 Topic:Climate
Related Subproject:A1
Subjects:Keywords: Precipitation, Humidity, Clouds
Geogr. Information Topic:Climatology/Meteorology/Atmosphere
File Details
Filename:crc_rainAtacama_v1.pdf
Data Type:Other - PDF
File Size:13.7 MB
Date:Created: 11.08.2023
Mime Type:application/pdf
Data Format:PDF
Language:English
Status:Completed
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Download Permission:Free
General Access and Use Conditions:According to the CRC1211DB data policy agreement.
Access Limitations:According to the CRC1211DB data policy agreement.
Licence:[CRC1211DB] Data policy agreement
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Specific Information - Presentation
Presenter:Jose Vicencio Veloso
Presentation Date:11th of August, 2023
Presentation Type:Talk
Event:Earth - Evolution at the dry limit
Event Type:Conference
Event Location:Köln, Deutschland
Event Duration:9th of August, 2023 - 11th of August, 2023
Event Website:https://sfb1211.uni-koeln.de/index.php/news/14-news/latest/222-international-conference-of-the-crc-1211-09-11-august-2023
Metadata Details
Metadata Creator:Jose Veloso
Metadata Created:04.12.2023
Metadata Last Updated:04.12.2023
Subproject:A1
Funding Phase:2
Metadata Language:English
Metadata Version:V50
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