首页> 外文期刊>Deep-Sea Research >Nearshore retention of upwelled waters north and south of Point Reyes (northern California)-Patterns of surface temperature and chlorophyll observed in CoOP WEST
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Nearshore retention of upwelled waters north and south of Point Reyes (northern California)-Patterns of surface temperature and chlorophyll observed in CoOP WEST

机译:雷耶斯角(加利福尼亚北部)北部和南部的上升水域的近岸滞留-在CoOP WEST中观测到的地表温度和叶绿素模式

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Retentive embayments can be found near capes in upwelling regions, where they stand out as relatively warm features with higher chlorophyll a concentrations than surrounding waters. Within the area of the "Wind Events and Shelf Transport" study site (WEST) from the Gulf of the Farallones to Point Arena (37.5-39°N and 122.5-124°W), we describe two retentive embayments, extending approximately 20 km north of Point Reyes, and 30 km south of Point Reyes in the northern Gulf of the Farallones. These areas are identifiable from chlorophyll a (SeaWiFS) and sea-surface temperature (MODIS) satellite radiometry. Additional data from moorings and drifters were used to further characterize these retentive features. The persistence of these features is on time scales between 2 and 10 days, determined from time-series analysis of mooring data for chlorophyll and temperature. The alongshore wind stress is negatively correlated with chlorophyll and temperature mooring values. The time scale of persistence of these retentive features was similar to both the upwelling-relaxation timescale and the timescale of phytoplankton bloom development. The WEST region is notable in that the spring and summer is subject to the strongest wind stress along the US west coast, yet the coastal waters are highly productive. Based on our observations, we suggest that the apparent persistence of high biomass coastal waters in this strongly advective and wind-dominated system may be partially explained by the presence of retentive features identified in this study.
机译:在上升流区的海角附近可以发现保持性浮游物,在那里它们表现为相对温暖的特征,叶绿素a的浓度高于周围水域。在从Farallones湾到Point Arena(北纬37.5-39°和北纬122.5-124°)的“风向和层架运输”研究站点(WEST)的区域内,我们描述了两个保持性延伸点,延伸约20公里在法拉隆北部海湾,雷耶斯角以北,雷耶斯角以南30公里。这些区域可通过叶绿素a(SeaWiFS)和海面温度(MODIS)卫星辐射测量法来识别。来自系泊设备和漂泊者的其他数据被用于进一步表征这些保持特征。这些特征的持续时间在2到10天之间,这是根据叶绿素和温度的系泊数据的时间序列分析确定的。沿海风应力与叶绿素和温度系泊值负相关。这些保持性特征的持续时间尺度与上升-松弛时间尺度和浮游植物开花发展的时间尺度相似。西部地区的显着之处在于,春季和夏季受到美国西海岸最强的风压,但沿海水域生产力很高。根据我们的观察,我们认为,在该强烈对流和以风为主的系统中,高生物量沿海水域的表观持久性可能部分由本研究中确定的保持性特征来解释。

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