Satellite-measured interannual variability of turbid river plumes off central-southern Chile: Spatial patterns and the influence of climate variability

被引:67
作者
Saldias, Gonzalo S. [1 ]
Largier, John L. [2 ]
Mendes, Renato [3 ]
Perez-Santos, Ivan [4 ]
Vargas, Cristian A. [5 ]
Sobarzo, Marcus [6 ,7 ]
机构
[1] Oregon State Univ, Coll Earth Ocean & Atmospher Sci, Corvallis, OR 97331 USA
[2] Univ Calif Davis, Bodega Marine Lab, Bodega Bay, CA USA
[3] Univ Aveiro, Dept Phys, CESAM, Aveiro, Portugal
[4] Univ Lagos, Ctr I Mar, Puerto Montt, Chile
[5] Univ Concepcion, Lab Funcionamiento Ecosistemas Acuat, Ctr Ciencias Ambientales EULA Chile, Concepcion, Chile
[6] Univ Concepcion, Dept Oceanog, Concepcion, Chile
[7] Univ Concepcion, Interdisciplinary Ctr Aquaculture Res INCAR, Concepcion, Chile
关键词
PARTICULATE ORGANIC-CARBON; COASTAL UPWELLING SYSTEM; STORMWATER RUNOFF PLUMES; SMALL MOUNTAINOUS RIVERS; OCEAN COLOR; CONTINENTAL-SHELF; FRESH-WATER; ATMOSPHERIC CORRECTION; CALIFORNIA BIGHT; CHESAPEAKE BAY;
D O I
10.1016/j.pocean.2016.07.007
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Ocean color imagery from MODIS (Moderate Resolution Imaging Spectroradiometer) onboard the Aqua platform is used to characterize the interannual variability of turbid river plumes off central-southern Chile. Emphasis is placed on the influence of climate fluctuations, namely El Nino Southern Oscillation (ENSO), the Pacific Decadal Oscillation (PDO), and the Antarctic Oscillation (AAO). Additional satellite data on wind, boat-based hydrographic profiles, and regional climate indices are used to identify the influence of climate variability on the generation of anomalous turbid river plumes. The evolution of salinity at a coastal station on the 90 m isobath between the Itata and Biobio Rivers shows a freshwater surface layer with salinity <32.5 and 5-10 m thick during major plume events in 2002, 2005 and 2006. Surface salinity minima are correlated with peaks in turbidy from the normalized water leaving radiance at 555 nm (nLw(555)), both representing turbid river plumes. EOF analysis reveals that major turbid plume events occurred primarily during warm phases of the ENSO and PDO, and negative phases of the AAO, when storm tracks are further north. Anomalously large turbid plumes extend long distances offshore (similar to 70-80 km), and individual plumes coalesce into a continuous plume along the coast that covers the entire continental shelf. Season-specific correlation analyses reveal an increased influence of the AAO on river plumes south of Punta Lavapie in spring-summer (negative correlation). North of this major cape, ENSO and PDO indices have a dominant influence on plumes with positive correlations with the nLw(555) signal in winter (and negative in summer). We discuss the biogeochemical implications of plume events and the importance of long-term and high-resolution ocean color observations for studying the temporal evolution of river plumes. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:212 / 222
页数:11
相关论文
共 71 条
[1]  
Aceituno P, 1990, REV SCO CHILEANA HID, V5, P7
[2]   Seasonal dynamics of the near-surface alongshore flow off central Chile [J].
Aguirre, Catalina ;
Pizarro, Oscar ;
Strub, Paul T. ;
Garreaud, Rene ;
Barth, John A. .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2012, 117
[3]  
[Anonymous], 2004, DATA ANAL METHODS PH
[4]   El Nino Modoki and its possible teleconnection [J].
Ashok, Karumuri ;
Behera, Swadhin K. ;
Rao, Suryachandra A. ;
Weng, Hengyi ;
Yamagata, Toshio .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2007, 112 (C11)
[5]   Spatially resolving ocean color and sediment dispersion in river plumes, coastal systems, and continental shelf waters [J].
Aurin, Dirk ;
Mannino, Antonio ;
Franz, Bryan .
REMOTE SENSING OF ENVIRONMENT, 2013, 137 :212-225
[6]   Riverine inorganic carbon flux and rate of biological uptake in the Mississippi River plume [J].
Cai, WJ .
GEOPHYSICAL RESEARCH LETTERS, 2003, 30 (02) :4-1
[7]   Trace metal fluxes to the ocean: The importance of high-standing oceanic islands [J].
Carey, AE ;
Nezat, CA ;
Lyons, WB ;
Kao, SJ ;
Hicks, DM ;
Owen, JS .
GEOPHYSICAL RESEARCH LETTERS, 2002, 29 (23) :14-1
[8]   Seasonal variations in the Amazon plume-related atmospheric carbon sink [J].
Cooley, S. R. ;
Coles, V. J. ;
Subramaniam, A. ;
Yager, P. L. .
GLOBAL BIOGEOCHEMICAL CYCLES, 2007, 21 (03)
[9]   Climatic sensitivity of streamflow timing in the extratropical western Andes Cordillera [J].
Cortes, Gonzalo ;
Vargas, Ximena ;
McPhee, James .
JOURNAL OF HYDROLOGY, 2011, 405 (1-2) :93-109
[10]   Contribution of small mountainous rivers to particulate organic carbon input in the Bay of Biscay [J].
Coynel, A ;
Etcheber, H ;
Abril, G ;
Maneux, E ;
Dumas, J ;
Hurtrez, JE .
BIOGEOCHEMISTRY, 2005, 74 (02) :151-171