Contributing slightly to the OLR′ trend is a small trend in OLRC′, which corresponds with a trend in TS′ of −1.8 K decade −1 (not shown).
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Sensitivity of Amazonian TOA flux diurnal cycle composite monthly variability to choice of reanalysis.
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For example, MERRA produces an increasing trend in CAPE of 403 J kg −1 decade −1 .