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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >The response of inorganic carbon distributions and dynamics to upwelling-favorable winds on the northern Gulf of Mexico during summer
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The response of inorganic carbon distributions and dynamics to upwelling-favorable winds on the northern Gulf of Mexico during summer

机译：夏季，墨西哥湾北部的无机碳分布和动力学对上升气流的响应

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摘要

Upwelling-favorable winds and an offshore-distributed Mississippi and Atchafalaya River plume trajectory were observed in summer 2009 in contrast to the mean conditions from 2002 to 2010 (upwelling-unfavorable Winds and an alongshore river plume trajectory), a set of conditions which was also observed in summer 2007. The responses of dissolved inorganic carbon (DIC) distributions and dynamics to upwelling-favorable winds are studied by comparing the contrasting conditions between summer 2009 and summer 2007 on the northern Gulf of Mexico. Patterns of surface water partial pressure of CO2 (PCO2), DIC, gamma C-13 in DIC, and total alkalinity (TA) determined in July 2009 and August 2007 were strongly related to river plume trajectories, and differed between the two summers.
机译：与2002年至2010年的平均条件（上升不利风和近岸河羽轨迹）相反，2009年夏季观测到上升气流有利以及密西西比河和阿查法拉亚河沿岸分布的羽流轨迹。通过比较墨西哥北部北部2009年夏季和2007年夏季之间的对比条件，研究了溶解无机碳（DIC）分布和动力学对上升气流的响应。 2009年7月和2007年8月确定的CO2（PCO2），DIC，DIC中的γC-13和总碱度（TA）的地表水分压模式与河羽轨迹密切相关，并且在两个夏季之间有所不同。

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