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1985年至2015年墨西哥湾北部大陆架夏季底层水温的变化趋势。

Trends in summer bottom-water temperatures on the northern Gulf of Mexico continental shelf from 1985 to 2015.

作者信息

Turner R Eugene, Rabalais Nancy N, Justić Dubravko

机构信息

Department of Oceanography and Coastal Sciences, Louisiana State University, Baton Rouge, Louisiana, United States of America.

Louisiana Universities Marine Consortium, Chauvin, Louisiana, United States of America.

出版信息

PLoS One. 2017 Sep 7;12(9):e0184350. doi: 10.1371/journal.pone.0184350. eCollection 2017.

DOI:10.1371/journal.pone.0184350
PMID:28880893
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5589215/
Abstract

We quantified trends in the 1985 to 2015 summer bottom-water temperature on the northern Gulf of Mexico (nGOM) continental shelf for data collected at 88 stations with depths ranging from 3 to 63 m. The analysis was supplemented with monthly data collected from 1963 to 1965 in the same area. The seasonal summer peak in average bottom-water temperature varied concurrently with air temperature, but with a 2- to 5-month lag. The summer bottom-water temperature declined gradually with depth from 30 oC at stations closest to the shore, to 20 oC at the offshore edge of the study area, and increased an average 0.051 oC y-1 between1963 and 2015. The bottom-water warming in summer for all stations was 1.9 times faster compared to the rise in local summer air temperatures, and 6.4 times faster than the concurrent increase in annual global ocean sea surface temperatures. The annual rise in average summer bottom-water temperatures on the subtropical nGOM continental shelf is comparable to the few published temperature trend estimates from colder environments. These recent changes in the heat storage on the nGOM continental shelf will affect oxygen and carbon cycling, spatial distribution of fish and shrimp, and overall species diversity.

摘要

我们对墨西哥湾北部(nGOM)大陆架1985年至2015年夏季底层水温的趋势进行了量化,这些数据来自88个深度在3至63米之间的站点。分析还补充了1963年至1965年在同一区域收集的月度数据。夏季平均底层水温的季节性峰值与气温同步变化,但有2至5个月的滞后。夏季底层水温从最靠近海岸的站点的30℃随深度逐渐下降到研究区域近海边缘的20℃,并且在1963年至2015年期间平均每年升高0.051℃。所有站点夏季底层水变暖速度比当地夏季气温上升速度快1.9倍,比同期全球海洋年海表温度上升速度快6.4倍。亚热带nGOM大陆架夏季平均底层水温的年上升幅度与少数已发表的较寒冷环境温度趋势估计值相当。nGOM大陆架近期的热储存变化将影响氧和碳循环、鱼虾的空间分布以及整体物种多样性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f24b/5589215/2e43547ec54c/pone.0184350.g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f24b/5589215/a3f0826e1cd5/pone.0184350.g001.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f24b/5589215/8b5a0e4bc074/pone.0184350.g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f24b/5589215/acbcd366b2a9/pone.0184350.g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f24b/5589215/a1ad73ef20a3/pone.0184350.g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f24b/5589215/2e43547ec54c/pone.0184350.g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f24b/5589215/a3f0826e1cd5/pone.0184350.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f24b/5589215/4a4d9cc658d6/pone.0184350.g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f24b/5589215/8b5a0e4bc074/pone.0184350.g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f24b/5589215/acbcd366b2a9/pone.0184350.g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f24b/5589215/a1ad73ef20a3/pone.0184350.g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f24b/5589215/2e43547ec54c/pone.0184350.g006.jpg

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