Varela R, Álvarez I, Santos F, deCastro M, Gómez-Gesteira M
EPhysLab, Departamento de Física Aplicada, Facultade de Ciencias, Universidade de Vigo, Ourense, España.
1] EPhysLab, Departamento de Física Aplicada, Facultade de Ciencias, Universidade de Vigo, Ourense, España [2] CESAM, Departamento de Física, Universidade de Aveiro, 3810-193, Aveiro, Portugal.
Sci Rep. 2015 May 8;5:10016. doi: 10.1038/srep10016.
Changes in coastal upwelling strength have been widely studied since 1990 when Bakun proposed that global warming can induce the intensification of upwelling in coastal areas. Whether present wind trends support this hypothesis remains controversial, as results of previous studies seem to depend on the study area, the length of the time series, the season, and even the database used. In this study, temporal and spatial trends in the coastal upwelling regime worldwide were investigated during upwelling seasons from 1982 to 2010 using a single wind database (Climate Forecast System Reanalysis) with high spatial resolution (0.3°). Of the major upwelling systems, increasing trends were only observed in the coastal areas of Benguela, Peru, Canary, and northern California. A tendency for an increase in upwelling-favourable winds was also identified along several less studied regions, such as the western Australian and southern Caribbean coasts.
自1990年巴昆提出全球变暖会导致沿海地区上升流增强以来,沿海上升流强度的变化已得到广泛研究。目前的风况趋势是否支持这一假设仍存在争议,因为先前研究的结果似乎取决于研究区域、时间序列的长度、季节,甚至所使用的数据库。在本研究中,利用具有高空间分辨率(0.3°)的单一风数据库(气候预测系统再分析),对1982年至2010年上升流季节期间全球沿海上升流状况的时空趋势进行了调查。在主要的上升流系统中,仅在本格拉、秘鲁、加那利和北加利福尼亚的沿海地区观测到上升趋势。在一些研究较少的地区,如澳大利亚西部和加勒比海南部海岸,也发现了有利于上升流的风有增加的趋势。