Journal of Geophysical Research Supporting Information for
Intraseasonal Variability of Upwelling in the Equatorial Eastern Indian Ocean Gengxin Chen1,2, Weiqing Han2, Yuanlong Li2, Dongxiao Wang1, Toshiaki Shinoda3
1
State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China
2Department 3
of Atmospheric and Oceanic Sciences, University of Colorado, Boulder, Colorado, USA
Department of Physical and Environmental Sciences, Texas A&M University–Corpus Christi, Corpus Christi, Texas, USA
Corresponding Author Gengxin Chen and Dongxiao Wang; State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China ; Email:
[email protected];
[email protected]
Contents of this file Figures S1 to S4
Introduction Four figures are uploaded as supporting information for this paper.
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Figure S1. Intraseasonal variability averaged in the SR for the modeled D20A (the upper panel) and SSTA (the lower panel) using 30-105d, 30-100d and 30-90d band pass filtered fields.
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Figure S2. Monthly climatology of (a) D20 and (b) SST from MR averaged in the EIO SR. Dashed horizontal lines in (a) and (b) are the mean D20 and SST with values of 118.3 m and 29.01 C.
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Figure S3. (a) Correlation coefficients between intraseasonal wind stress curl at each grid point and intraseasonal D20A averaged in the SR from the MR in summer-fall. Only grid points with confidence level above 95% are plotted. (b) Same as (a) but for intraseasonal wind stress curl and intraseasonal SSTA. (c) Same as (a) but for winter-spring. (d) Same as (b) but for winter-spring.
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Figure S4. Same as Figure S3 but for correlation coefficients of intraseasonal wind speed with D20A and SSTA.
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