巴塔哥尼亚北部奇洛埃内海浑浊淡水羽流的时空变化

IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Raúl P. Flores , Carlos Lara , Gonzalo S. Saldías , Sebastián I. Vásquez , Alonso Roco
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引用次数: 5

摘要

巴塔哥尼亚北部的特点是有多条河流向沿海海洋排放大量淡水,形成影响水文和生态过程的大型河流羽流。本研究首次利用MODIS(中分辨率成像光谱仪)卫星海洋颜色数据表征了巴塔哥尼亚北部内水浑浊淡水羽流的季节和年际变化,重点研究了其与河流流量和大尺度气候变化的联系。以645 nm为中心的表面反射率产品的浊度信号,Rrs(645),与河流流量数据的峰值和基于船的剖面和水面浮标的表面盐度最小值有很好的相关性,验证了其用于识别该地区浑浊河流羽流的用途。Rrs(645)的季节气候学表现为全年存在较大的河流羽流,其变化主要与河流流量有关。通过对低流量和高流量条件下的Rrs(645)场的分析,可以确定一个阈值,以描绘羽流锋面并确定羽流发生的概率。EOF分析揭示了羽流变化的主要模式,与沿海边缘和较深水域之间的浊度差异以及整个研究区域内大型河流羽流的同相变化有关。最大的羽流事件发生在2008年,在ENSO (La Niña)和PDO的负(冷)阶段,而SAM的正阶段。EOF分析很好地捕捉到了2016年发生在ENSO (El Niño)、PDO和SAM正相期间的严重干旱事件,其特征是Rrs(645)信号出现了较大的负异常。总体而言,Rrs(645)的月异常与ENSO、PDO和SAM指数之间存在复杂的共变,突出了该地区气候调节的异质性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Spatio-temporal variability of turbid freshwater plumes in the Inner Sea of Chiloé, northern Patagonia

Northern Patagonia is characterized by multiple rivers that discharge considerable amounts of freshwater into the coastal ocean, forming large river plumes that influence hydrographic and ecological processes. In this study, we use satellite ocean color data from MODIS (Moderate Resolution Imaging Spectroradiometer) to characterize the seasonal and interannual variability of turbid freshwater plumes in the inner waters of northern Patagonia for the first time, with a focus on the connections to river discharge and large-scale climatic variability. The turbidity signal from the surface reflectance product centered at 645 nm, Rrs(645), correlates well with peaks in river discharge data and surface salinity minima from boat-based profiles and a surface buoy, validating its use for the identification of turbid river plumes in the region. The seasonal climatology of Rrs(645) showed the presence of large river plumes throughout the year, with variability associated mainly to that of river discharge. Analysis of Rrs(645) fields under low and high discharge conditions allowed for the identification of a threshold value to delineate plume fronts and determine the probability of plume occurrence. EOF analysis reveals the dominant modes of plume variability, associated to turbidity differences between the coastal margin and deeper waters and to in-phase variability of large river plumes throughout the study area. The largest plume event occurred in year 2008, during negative (cold) phases of ENSO (La Niña) and PDO but a positive phase of SAM. The severe drought event of 2016 that occurred during positives phase of ENSO (El Niño), PDO and SAM is well captured by the EOF analysis and is characterized by large negative anomalies in the Rrs(645) signal. In general, complex co-variations are observed between monthly anomalies of Rrs(645) and the ENSO, PDO and SAM indices, highlighting the heterogeneity of climatic regulation in the region.

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来源期刊
Journal of Marine Systems
Journal of Marine Systems 地学-地球科学综合
CiteScore
6.20
自引率
3.60%
发文量
81
审稿时长
6 months
期刊介绍: The Journal of Marine Systems provides a medium for interdisciplinary exchange between physical, chemical and biological oceanographers and marine geologists. The journal welcomes original research papers and review articles. Preference will be given to interdisciplinary approaches to marine systems.
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