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Near-surface phytoplankton distribution in the western Intra-Americas Sea: The influence of El Nino and weather events

机译:美洲西部海域近地表浮游植物分布:厄尔尼诺现象和天气事件的影响

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The space-rime variation of phytoplankton pigments in the western Intra-Americas Sea (IAS), in the vicinity of the island of Cuba, is examined using digital images obtained with the Coastal Zone Color Scanner sensor flown aboard the Nimbus 7 satellite from 1978 to 1986. The results are compared to historical in situ hydrographic observations. A marked seasonality in pigment concentration was observed in waters around Cuba, with an average of 0.07 mg m(-3) in summer (April-September) and 0.13 mg m-3 during winter (October-March). The range of variation in pigment concentration was larger in the Gulf of Mexico relative to the western Caribbean Sea. We identified four biogeographical areas on the basis of groups of pixels with similar patterns of time variability. These are area I: southwest of Cuba, Yucatan Channel, and Florida Strait; area II: central Gulf of Mexico; area III: east of Cuba; and area IV: central Caribbean Sea, south of Jamaica and Hispaniola. Two major meteorological events led to anomalies in the seasonal cycle of pigment concentrations. During El Nino-Southern Oscillation (ENSO) of 1982-1983, positive anomalies were observed in the pigment concentration in the western IAS during winter months. This was associated with intense mixing of the water column by higher-frequency and stronger winds associated with cold fronts. ENSO 1952-1983 therefore had a fertilizing effect on the IAS region. Another positive anomaly was observed in 1980-1981, a non-ENSO period that featured higher hurricane and extratropical low-pressure activity. [References: 61]
机译:利用从1978年至2007年间在Nimbus 7卫星上飞行的Coastal Zone Color Scanner传感器获得的数字图像,研究了古巴岛附近美洲西部海域(IAS)中浮游植物色素的空间边缘变化。 1986年。将结果与历史现场水文观测结果进行比较。在古巴周围水域观察到明显的色素浓度季节性变化,夏季(4月至9月)平均为0.07 mg m(-3),冬季(10月至3月)平均为0.13 mg m-3。相对于西加勒比海,墨西哥湾的颜料浓度变化范围更大。我们根据具有相似时间可变模式的像素组确定了四个生物地理区域。这些是I区:古巴西南,尤卡坦海峡和佛罗里达海峡;第二区:墨西哥湾中部;第三区:古巴以东;第四区:中部加勒比海,牙买加和伊斯帕尼奥拉以南。两次主要的气象事件导致色素浓度的季节性周期异常。在1982年至1983年的厄尔尼诺-南方涛动(ENSO)期间,在冬季,IAS西部的色素浓度出现了正异常。这是由于与冷锋相关的高频和强风使水柱剧烈混合。因此ENSO 1952-1983对IAS地区产生了施肥作用。在1980年至1981年观察到另一个正异常,这是一个非ENSO时期,其特征是飓风和温带低压活动较高。 [参考:61]

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