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Ocean Color Response to an Episode of Heavy Rainfall In the Lagoon of New Caledonia

机译:海洋颜色对新喀里多尼亚泻湖暴雨的反应

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Inherent optical properties (IOPs) and remote sensing reflectance were measured in the southern part of the lagoon of New Caledonia during the VALHYBIO cruise (March-April 2008). The goal was to validate satellite chlorophyll data from MODIS and MERIS and to validate simulations of surface chlorophyll by a biogeochemical model. Physical parameters were collected from a Seabird CTD. Particulate and detritus absorption were measured with the filter pad technique. Backscattering was measured with a Hydroscat-6. Mapping of IOPs and Rrs were done for the whole southern lagoon area and compared with pigment maps. The cruise provided a description of the IOPs in different water types including bays, open ocean waters, mid-shelf lagoon, and above reefs. With respect to climatology, the heavy rainfall episode of March-April 2008 resulted in a large increase in chlorophyll-a concentration (by a factor of 3) attributed to increased nutrient availability from land drainage. Low backscattering ratios characterized the chlorophyll-rich plumes associated with the nutrient increase. The data are useful for the development of a specific algorithm for chlorophyll concentration retrieval by satellite in all oligotrophic lagoons during dry and wet seasons.
机译:在VALHYBIO航行期间(2008年3月至4月),在新喀里多尼亚泻湖的南部测量了固有的光学特性(IOP)和遥感反射率。目的是验证来自MODIS和MERIS的卫星叶绿素数据,并通过生物地球化学模型验证表面叶绿素的模拟。物理参数是从Seabird CTD收集的。用滤垫技术测量颗粒和碎屑吸收。使用Hydroscat-6测量背向散射。对整个南部泻湖地区的IOP和Rrs进行了制图,并与色素图进行了比较。巡游提供了对不同水类型的IOP的描述,包括海湾,开阔海水,中层泻湖和礁石之上。在气候方面,2008年3月至4月的暴雨导致叶绿素a浓度大幅增加(增加了3倍),这归因于土地排水带来的养分增加。低反向散射比的特征在于与营养增加相关的富含叶绿素的羽流。该数据对于开发在干旱和潮湿季节在所有贫营养泻湖中通过卫星检索叶绿素浓度的特定算法很有用。

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