Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1007/s00382-019-04907-w |
Salinity frontogenesis/frontolysis in the northeastern subtropical Pacific region | |
Ohishi, Shun1; Katsura, Shota2; Aiki, Hidenori1 | |
2019-11-01 | |
发表期刊 | CLIMATE DYNAMICS |
ISSN | 0930-7575 |
EISSN | 1432-0894 |
出版年 | 2019 |
卷号 | 53页码:5927-5943 |
文章类型 | Article |
语种 | 英语 |
国家 | Japan; USA |
英文摘要 | Detailed mechanisms of reinforcement/relaxation of a sea surface salinity front, i.e. frontogenesis/frontolysis, in the northeastern subtropical Pacific region are investigated using observational datasets. Throughout the year, meridional shears of zonal wind induce meridional ageostrophic convergence around the front. Saltier water is advected on the southern side than the northern side, and thus the convergence contributes to frontogenesis. The evaporation and precipitation gradients also strengthen the front, because higher sea surface temperatures on the southern side induce stronger evaporation through the formation of higher surface saturated specific humidity, and because the precipitation rate is low in the southern region in association with the subtropical high of the atmosphere. However, in summer-autumn when the mixed layer is seasonally thin and evaporation exceeds precipitation, the frontogenesis by the freshwater flux gradient is damped by the mixed layer depth (MLD) gradient. This is attributed to the thicker mixed layer south of the front being less sensitive to freshwater fluxes. During the mixed-layer deepening phase, the mixed layer on the southern side entrains lower salinity water from the lower layer, and thus the entrainment relaxes the front. Therefore, it is shown that the gradients of ageostrophic advection, evaporation, and precipitation result in frontogenesis, while those of MLD and entrainment cause frontolysis. Furthermore, a metric that quantifies the relative importance of the horizontal gradients of freshwater fluxes and MLD for salinity frontogenesis/frontolysis is proposed. Over the large domain, contribution from the horizontal gradient of freshwater fluxes dominates over that of MLD. |
英文关键词 | Sea surface salinity front Frontogenesis/frontolysis The northeastern subtropical Pacific Freshwater flux frontogenesis metric |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000493469900044 |
WOS关键词 | SURFACE HEAT-FLUX ; BARRIER-LAYER FORMATION ; RETURN CURRENT REGION ; MIXED-LAYER ; MODE WATER ; TOGA DECADE ; OCEAN ; FRONTOLYSIS ; MECHANISMS ; PROGRAM |
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/187932 |
专题 | 气候变化 |
作者单位 | 1.Nagoya Univ, Inst Space Earth Environm Res, Chikusa Ku, Furo Cho, Nagoya, Aichi 4648601, Japan; 2.Univ Calif San Diego, Scripps Inst Oceanog, San Diego, CA 92103 USA |
推荐引用方式 GB/T 7714 | Ohishi, Shun,Katsura, Shota,Aiki, Hidenori. Salinity frontogenesis/frontolysis in the northeastern subtropical Pacific region[J]. CLIMATE DYNAMICS,2019,53:5927-5943. |
APA | Ohishi, Shun,Katsura, Shota,&Aiki, Hidenori.(2019).Salinity frontogenesis/frontolysis in the northeastern subtropical Pacific region.CLIMATE DYNAMICS,53,5927-5943. |
MLA | Ohishi, Shun,et al."Salinity frontogenesis/frontolysis in the northeastern subtropical Pacific region".CLIMATE DYNAMICS 53(2019):5927-5943. |
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