Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.gloplacha.2020.103192 |
Water vapor variability in the Atacama Desert during the 20th century | |
Boehm, Christoph; Reyers, Mark; Schween, Jan Herbert; Crewell, Susanne | |
通讯作者 | Bohm, C |
来源期刊 | GLOBAL AND PLANETARY CHANGE
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ISSN | 0921-8181 |
EISSN | 1872-6364 |
出版年 | 2020 |
卷号 | 190 |
英文摘要 | This study focuses on integrated water vapor (IWV) which is the main source for precipitation, fog and dew formation in the Atacama Desert in northern Chile. In order to study its long-term variability, a consistent meteorological record is needed. Here, we utilize the European Centre for Medium-Range Weather Forecasts' reanalysis ERA-20C which provides IWV among other atmospheric variables over the course of the entire 20th century (1900-2010). In this two fold study, we first present a validation of ERA-20C IWV for the Atacama and the bordering southeast Pacific region. Comparisons to satellite observations, i.e. the Hamburg Ocean Atmosphere Parameters and Fluxes from Satellite data record and the Moderate Resolution Imaging Spectroradiometer measurements, for overlapping time periods prove the suitability of ERA-20C to study IWV variability. Assessment of the observation feedback in ERA-20C reveals a higher uncertainty for the beginning of the 20th century when fewer observations are assimilated. Nevertheless, departures of the assimilated observations do not show a systematic bias in space or time supporting suitability of ERA-20C for long-term investigations. In the second part of the study, we describe the IWV variability over the course of the 20th century. Deviations from the long-term mean greater than 30% are found on an inter-annual time scale over the continental Atacama. Furthermore, we investigate potential drivers of the IWV variability such as the Pacific Decadal Oscillation (PDO) and the El Nino Southern Oscillation (ENSO) phenomenon. The relationship between the local IWV and these large scale indices depends on region and season. For instance, during austral summer, La Nina conditions yield overall greater IWV variability in the Atacama allowing both drier and even more pronounced wetter extremes than El Nino conditions. |
英文关键词 | Water cycle Integrated water vapor ERA-20C Atacama Hydrological cycle Moisture transport |
类型 | Article |
语种 | 英语 |
开放获取类型 | hybrid |
收录类别 | SCI-E |
WOS记录号 | WOS:000536927700007 |
WOS关键词 | SOUTHEAST PACIFIC ; VOCALS-REX ; CLIMATE ; PRECIPITATION ; REANALYSIS ; OSCILLATION ; CIRCULATION ; MECHANISMS ; ALTIPLANO ; ANOMALIES |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS研究方向 | Physical Geography ; Geology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/324589 |
作者单位 | [Boehm, Christoph; Reyers, Mark; Schween, Jan Herbert; Crewell, Susanne] Univ Cologne, Inst Geophys & Meteorol, Cologne, Germany |
推荐引用方式 GB/T 7714 | Boehm, Christoph,Reyers, Mark,Schween, Jan Herbert,et al. Water vapor variability in the Atacama Desert during the 20th century[J],2020,190. |
APA | Boehm, Christoph,Reyers, Mark,Schween, Jan Herbert,&Crewell, Susanne.(2020).Water vapor variability in the Atacama Desert during the 20th century.GLOBAL AND PLANETARY CHANGE,190. |
MLA | Boehm, Christoph,et al."Water vapor variability in the Atacama Desert during the 20th century".GLOBAL AND PLANETARY CHANGE 190(2020). |
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