Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1002/2017JD026791 |
The isotopic composition of near-surface water vapor at the Maido observatory (Reunion Island, southwestern Indian Ocean) documents the controls of the humidity of the subtropical troposphere | |
Guilpart, Etienne1; Vimeux, Francoise1,2; Evan, Stephanie3; Brioude, Jerome3; Metzger, Jean-Marc4; Barthe, Christelle3; Risi, Camille5; Cattani, Olivier2 | |
2017-09-27 | |
发表期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
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ISSN | 2169-897X |
EISSN | 2169-8996 |
出版年 | 2017 |
卷号 | 122期号:18 |
文章类型 | Article |
语种 | 英语 |
国家 | France |
英文摘要 | We present a 1 year long record of the isotopic composition of near-surface water vapor (delta O-18(v)) at the Maido atmospheric observatory (Reunion Island, Indian Ocean, 22 degrees S, 55 degrees E) from 1 November 2014 to 31 October 2015, using wavelength-scanned cavity ring down spectroscopy. Except during cyclone periods where delta O-18(v) is highly depleted (-20.5%), a significant diurnal variability can be seen on both delta O-18(v) and q(v) with enriched (depleted) water vapor (mean delta O-18(v) is -13.4% (-16.6%)) and moist (dry) conditions (mean q(v) is 9.7 g/kg (6.4 g/kg)) during daytime (nighttime). We show that d18Ov diurnal cycle arises from mixing processes for 65% of cases with two distinct sources of water vapor. We suggest that delta O-18(v) diurnal cycle is controlled by an interplay of thermally driven land-sea breezes and upslope-downslope flows, bringing maritime air to the observatory during daytime, whereas at night, the observatory is above the atmospheric boundary layer and samples free tropospheric air. Interestingly, delta O-18(v) record also shows that some nights (15%) are extremely depleted (mean delta O-18(v) is -21.4%). They are among the driest of the record (mean q(v) is 2.9 g/kg). Based on different modeling studies, we suggest that extreme nocturnal isotopic depletions are caused by large-scale atmospheric transport and subsidence of dry air masses from the upper troposphere to the surface, induced by the subtropical westerly jet. |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000416388000006 |
WOS关键词 | DEUTERIUM EXCESS ; IN-SITU ; SEASONAL-VARIATIONS ; HDO/H2O RATIOS ; BOUNDARY-LAYER ; LA FOURNAISE ; PRECIPITATION ; TRANSPORT ; OZONE ; PITON |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/32349 |
专题 | 气候变化 |
作者单位 | 1.UVSQ, Lab Sci Climat & Environnm, IPSL, UMR 8212,CEA,CNRS, Gif Sur Yvette, France; 2.UM, UMR 5569, Inst Rech Dev, Lab Hydrosci Montpellier,CNRS,IRD, Montpellier, France; 3.Univ La Reunion, CNRS, UMR CNRS 8105, Lab Atmosphere & Cyclones,Meteo France, Saint Denis De La Reunio, France; 4.Univ La Reunion, UMS 3365, Observ Sci, CNRS,Meteo France, Saint Denis De La Reunio, France; 5.UPMC, UMR 8539, Lab Meteorol Dynam, IPSL,Sorbonne Univ,CNRS,ENS,X, Paris, France |
推荐引用方式 GB/T 7714 | Guilpart, Etienne,Vimeux, Francoise,Evan, Stephanie,et al. The isotopic composition of near-surface water vapor at the Maido observatory (Reunion Island, southwestern Indian Ocean) documents the controls of the humidity of the subtropical troposphere[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2017,122(18). |
APA | Guilpart, Etienne.,Vimeux, Francoise.,Evan, Stephanie.,Brioude, Jerome.,Metzger, Jean-Marc.,...&Cattani, Olivier.(2017).The isotopic composition of near-surface water vapor at the Maido observatory (Reunion Island, southwestern Indian Ocean) documents the controls of the humidity of the subtropical troposphere.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,122(18). |
MLA | Guilpart, Etienne,et al."The isotopic composition of near-surface water vapor at the Maido observatory (Reunion Island, southwestern Indian Ocean) documents the controls of the humidity of the subtropical troposphere".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 122.18(2017). |
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