Observed Ocean Bottom Temperature Variability at Four Sites in the Northwestern Argentine Basin: Evidence of Decadal Deep/Abyssal Warming Amidst Hourly to Interannual Variability During 2009-2019

被引:25
作者
Meinen, Christopher S. [1 ]
Perez, Renellys C. [1 ]
Dong, Shenfu [1 ]
Piola, Alberto R. [2 ,3 ,4 ]
Campos, Edmo [5 ,6 ]
机构
[1] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA
[2] Serv Hidrog Naval, Buenos Aires, DF, Argentina
[3] Univ Buenos Aires, Buenos Aires, DF, Argentina
[4] Consejo Nacl Invest Cient & Tecn, Inst Francoargentino Estudios Clima & Sus Impacto, Buenos Aires, DF, Argentina
[5] Univ Sao Paulo, Oceanog Inst, Sao Paulo, Brazil
[6] Amer Univ Shatjah, Sch Arts & Sci, Dept Biol Chem & Environm Sci, Sharjah, U Arab Emirates
基金
巴西圣保罗研究基金会;
关键词
WESTERN BOUNDARY CURRENT; MERIDIONAL OVERTURNING CIRCULATION; CURRENT TRANSPORT VARIABILITY; SEA-LEVEL RISE; SOUTH ATLANTIC; NORTH-ATLANTIC; GULF-STREAM; GLOBAL HEAT; DEEP; 34.5-DEGREES-S;
D O I
10.1029/2020GL089093
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Consecutive multiyear records of hourly ocean bottom temperature measurements are merged to produce new decade-long time series at four depths ranging from 1,360 to 4,757 m within the northwest Argentine Basin at 34.5 degrees S. Energetic temperature variations are found at a wide range of time scales. All sites exhibit fairly linear warming trends of approximately 0.02-0.04 degrees C per decade over the period 2009-2019, although the trends are only statistically different from zero at the two deepest sites at depths of similar to 4,500-4,800 m. Near-bottom temperatures from independent conductivity-temperature-depth profiles collected at these same locations every 6-24 months over the same decade show roughly consistent trends. Based on the distribution of spectral energies at the deepest sites and a Monte Carlo-style analysis, sampling at least once per year is necessary to capture the significant warming trends over this decade to within 50% error bars at a 95% confidence limit.
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页数:8
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