Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.5194/acp-19-12235-2019 |
Controls on the water vapor isotopic composition near the surface of tropical oceans and role of boundary layer mixing processes | |
Risi, Camille1; Galewsky, Joseph2; Reverdin, Gilles3; Brient, Florent4 | |
2019-10-02 | |
发表期刊 | ATMOSPHERIC CHEMISTRY AND PHYSICS
![]() |
ISSN | 1680-7316 |
EISSN | 1680-7324 |
出版年 | 2019 |
卷号 | 19期号:19页码:12235-12260 |
文章类型 | Article |
语种 | 英语 |
国家 | France; USA |
英文摘要 | Understanding what controls the water vapor isotopic composition of the sub-cloud layer (SCL) over tropical oceans (delta D-0) is a first step towards understanding the water vapor isotopic composition everywhere in the troposphere. We propose an analytical model to predict delta D-0 motivated by the hypothesis that the altitude from which the free tropospheric air originates (z(orig)) is an important factor: when the air mixing into the SCL is lower in altitude, it is generally moister, and thus it depletes the SCL more efficiently. We extend previous simple box models of the SCL by prescribing the shape of delta D vertical profiles as a function of humidity profiles and by accounting for rain evaporation and horizontal advection effects. The model relies on the assumption that delta D profiles are steeper than mixing lines, and that the SCL is at steady state, restricting its applications to timescales longer than daily. In the model, delta D-0 is expressed as a function of z ong , humidity and temperature profiles, surface conditions, a parameter describing the steepness of the delta D vertical gradient, and a few parameters describing rain evaporation and horizontal advection effects. We show that delta D-0 does not depend on the intensity of entrainment, in contrast to several previous studies that had hoped that delta D-0 measurements could help estimate this quantity. Based on an isotope-enabled general circulation model simulation, we show that delta D-0 variations are mainly controlled by mid-tropospheric depletion and rain evaporation in ascending regions and by sea surface temperature and z(orig) in subsiding regions. In turn, could SDo measurements help estimate z ong and thus discriminate between different mixing processes? For such isotope-based estimates of z(ori)(g) to be useful, we would need a precision of a few hundred meters in deep convective regions and smaller than 20 m in stratocumulus regions. To reach this target, we would need daily measurements of delta D in the mid-troposphere and accurate measurements of delta D-0 (accuracy down to 0.1 parts per thousand in the case of stratocumulus clouds, which is currently difficult to obtain). We would also need information on the horizontal distribution of delta D to account for horizontal advection effects, and full delta D profiles to quantify the uncertainty associated with the assumed shape for delta D profiles. Finally, rain evaporation is an issue in all regimes, even in stratocumulus clouds. Innovative techniques would need to be developed to quantify this effect from observations. |
领域 | 地球科学 |
收录类别 | SCI-E |
WOS记录号 | WOS:000488979300004 |
WOS关键词 | LARGE-EDDY SIMULATIONS ; CLOUD-TOP ENTRAINMENT ; COHERENT STRUCTURES ; STABLE-ISOTOPES ; ANTARCTIC PRECIPITATION ; SUBSIDING SHELLS ; DEUTERIUM EXCESS ; CLIMATE-CHANGE ; DELTA-D ; MODEL |
WOS类目 | Environmental Sciences ; Meteorology & Atmospheric Sciences |
WOS研究方向 | Environmental Sciences & Ecology ; 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/187568 |
专题 | 地球科学 |
作者单位 | 1.Sorbonne Univ, Lab Meteorol Dynam, CNRS, IPSL, Paris, France; 2.Univ New Mexico, Dept Earth & Planetary Sci, Albuquerque, NM 87131 USA; 3.Sorbonne Univ, IPSL, LOCEAN, CNRD,IRD,MNHN, Paris, France; 4.Univ Toulouse, CNRS, CNRM, Meteo France, Toulouse, France |
推荐引用方式 GB/T 7714 | Risi, Camille,Galewsky, Joseph,Reverdin, Gilles,et al. Controls on the water vapor isotopic composition near the surface of tropical oceans and role of boundary layer mixing processes[J]. ATMOSPHERIC CHEMISTRY AND PHYSICS,2019,19(19):12235-12260. |
APA | Risi, Camille,Galewsky, Joseph,Reverdin, Gilles,&Brient, Florent.(2019).Controls on the water vapor isotopic composition near the surface of tropical oceans and role of boundary layer mixing processes.ATMOSPHERIC CHEMISTRY AND PHYSICS,19(19),12235-12260. |
MLA | Risi, Camille,et al."Controls on the water vapor isotopic composition near the surface of tropical oceans and role of boundary layer mixing processes".ATMOSPHERIC CHEMISTRY AND PHYSICS 19.19(2019):12235-12260. |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论