Relative role of wind forcing and riverine nutrient input on the extent of hypoxia in the northern Gulf of Mexico
Article first published online: 3 MAY 2012
Copyright 2012 by the American Geophysical Union
Geophysical Research Letters
Volume 39, Issue 9, May 2012
How to Cite
2012), Relative role of wind forcing and riverine nutrient input on the extent of hypoxia in the northern Gulf of Mexico, Geophys. Res. Lett., 39, L09601, doi:10.1029/2012GL051192., , and (
- Issue published online: 3 MAY 2012
- Article first published online: 3 MAY 2012
- Manuscript Accepted: 29 MAR 2012
- Manuscript Revised: 27 MAR 2012
- Manuscript Received: 16 FEB 2012
- NOAA-CSCOR. Grant Number: NGOMEX2009-NAO9NOS4780208
Auxiliary material for this article contains tables and figures relating to the historical data set used for statistical analysis, and part of statistical analysis results, including bootstrap analysis to determine the robustness of regression and correlation analysis to find the maximum correlation between the hypoxic area and duration of westerly wind.
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|grl29051-sup-0001-readme.txt||plain text document||7K||readme.txt|
|grl29051-sup-0002-ts01.txt||plain text document||1K||Table S1. Data used in the regression analysis presented in the paper.|
|grl29051-sup-0003-ts02.txt||plain text document||1K||Table S2. Bootstrap analysis results.|
|grl29051-sup-0004-fs01.eps||PS document||8K||Figure S1. The correlation coefficient between the hypoxic area and the duration of west wind as a function of the window length.|
|grl29051-sup-0005-fs02.eps||PS document||25456K||Figure S2. The relationship between hypoxic area and F_11, and F_11 + t_Uwind, and F_May, and F_May + t_Uwind, and F_Spring, and F_Spring + t_Uwind for 1993–2010 period.|
|grl29051-sup-0006-fs03.eps||PS document||28637K||Figure S3. Spatial averaged east-west wind from 1985–2010.|
|grl29051-sup-0007-fs04.eps||PS document||8494K||Figure S4. The surface salinity and chlorophyll concentrations under the downwelling favorable wind, the beginning of upwelling favorable wind, and the end of upwelling favorable wind period.|
|grl29051-sup-0008-txts01.pdf||PDF document||28K||Text S1. Variation of surface salinity and chlorophyll distribution with the persistent westerly wind in 2009|
|grl29051-sup-0009-t01.txt||plain text document||1K||Tab-delimited Table 1.|
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