Fig. 5
From: Late Holocene slowdown of the Indian Ocean Walker circulation
LGM climate anomalies in the Indian Ocean region as simulated by CCSM3 and FGOALS-g1.0. Shown are LGM anomalies (annual mean) relative to pre-industrial control runs for ΔT (defined as ocean temperature difference between surface and 70 m as a measure for tropical thermocline depth) and low-level (925 hPa) wind (a, c) and vertical velocity (ω) between 5° S and 5° N (b, d) for the two climate models with greatest LGM thermocline deepening in the eastern equatorial Indian Ocean and strongest equatorial westerly wind anomalies (Nos. 13 and 14 in Fig. 4), CCSM3 (a, b) and FGOALS-g1.0 (c, d). Grey box in a shows the region for calculating area-averaged ΔT in all the models in Fig. 4, while the grey box in c shows the region for averaging U eq. Modern coastlines are drawn in a and c for better orientation
