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POC algorithms based on spectral remote sensing data and its temporal and spatial variability in the Gulf of Mexico

机译:基于光谱遥感数据的POC算法及其在墨西哥湾的时空变化

摘要

This dissertation consists of three studies dealing with particulate organic carbon(POC). The first study describes the temporal and spatial variability of particulate matter(PM) and POC, and physical processes that affect the distribution of PM and POC withsynchronous remote sensing data. The purpose of the second study is to develop POCalgorithms in the Gulf of Mexico based on satellite data using numerical methods and tocompare POC estimates with spectral radiance. The purpose of the third study is toinvestigate climatological variations from the temporal and spatial POC estimates basedon SeaWiFS spectral radiance and physical processes, and to determine the physicalmechanisms that affect the distribution of POC in the Gulf of Mexico.For the first and second studies, hydrographic data from the Northeastern Gulf ofMexico (NEGOM) study were collected on each of 9 cruises from November 1997 toAugust 2000 across 11 lines. Remotely sensed data sets were obtained from NASA andNOAA using algorithms that have been developed for interpretation of ocean color datafrom various satellite sensors. For the third study, we use the time-series of POCestimates, sea surface temperature (SST), sea surface height anomaly (SSHA), sea surface wind (SSW), and precipitation rate (PR) that might cause climatologicalvariability and physical processes.The distribution of surface PM and POC concentrations were affected by one ormore factors such as river discharge, wind stress, stratification, and the LoopCurrent/Eddies. To estimate POC concentration, empirical and model-based approacheswere used using regression and principal component analysis (PCA) methods. We testedsimulated data for reasonable and suitable algorithms in Case 1 and Case 2 waters.Monthly mean values of POC concentrations calculated with PCA algorithms.The spatial and temporal variations of POC and physical forcing data were analyzedwith the empirical orthogonal function (EOF) method. The results showed variations inthe Gulf of Mexico on both annual and inter-annual time scales.
机译:本文由三项涉及颗粒有机碳(POC)的研究组成。第一项研究描述了颗粒物(PM)和POC的时间和空间变异性,以及通过同步遥感数据影响PM和POC分布的物理过程。第二项研究的目的是使用数值方法基于卫星数据开发墨西哥湾的POC算法,并将POC估计值与光谱辐射度进行比较。第三项研究的目的是根据基于SeaWiFS光谱辐射度和物理过程的时空POC估计值调查气候变化,并确定影响墨西哥湾POC分布的物理机制。从墨西哥东北湾(NEGOM)研究获得的数据是从1997年11月至2000年8月的9条航线中的11条航线上收集的。从NASA和NOAA获得的遥感数据集使用的算法已开发出来,用于解释来自各种卫星传感器的海洋颜色数据。对于第三项研究,我们使用可能引起气候变化和物理过程的POC估计值,海面温度(SST),海面高度异常(SSHA),海面风(SSW)和降水率(PR)的时间序列。表面PM和POC浓度的分布受一个或多个因素的影响,例如河流流量,风应力,分层和LoopCurrent / Eddies。为了估计POC浓度,使用了基于经验和基于模型的方法,使用了回归和主成分分析(PCA)方法。我们在案例1和案例2的水域中测试了模拟数据的合理和合适算法。使用PCA算法计算POC浓度的每月平均值。使用经验正交函数(EOF)方法分析了POC的时空变化和物理强迫数据。结果表明,墨西哥湾的年度和年度时间尺度都不同。

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    Son Young Baek;

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  • 年度 2007
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