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. 2015 Jan 22;282(1799):20140650. doi: 10.1098/rspb.2014.0650

Table 1.

Temperature conditions during the high temperature anomaly in 2010 summarized for the exposed west (W) and sheltered east (E) sites; Tachai W (TW), Payang W (PW), Miang W (MW), Similan W (SiW), Racha W (RW), Surin W (SuW), Bon W (BW), Racha E (RE), Payang E (PE), Miang E (ME), Similan E (SiE) and Surin E (SuE). Temperature values include mean, maximum (max) and minimum (min) temperature recorded during this period. LAIW cooling intensities are calculated as degree-day cooling (DDC) below the NOAA bleaching threshold (30.62°C). Degree heating weeks (DHW) derived from satellite (DHWs) and field data (DHWf) reflect differences in heat anomaly observed at the sea surface and in 15 m water depth.

sites exposed
sheltered
TW PWa MW SiWa RW SuW BW REb PEa ME SiEa SuE
mean (°C) 30.3 30.3 30.3 30.5 30.6 30.7 30.6 30.8
max (°C) 32.1 31.9 31.8 32.2 32.3 32.3 32.4 32.2
min (°C) 22.1 22.1 24.5 23.9 23.4 25.7 26.3 27.6
DDC (°Cd) −16.8 −19.2 −15.0 −10.6 −7.7 −10.1 −3.9 −1.5
DHWs 5.2 4 4 4 5.7 6.8 5.2 5.7 4 4 4 6.8
DHWf 2.4 2.3 2.3 2.3 1.2 5.4 6.2 6 7.8 7.8 7.8 9

aPayang E, Payang W, Similan E and Similan W data are unavailable. For calculation of DHWf, temperature data were taken from corresponding E and W sites of Miang, respectively. For justification cf. Schmidt et al. [15].

bRacha E temperature record was available only for 20 and 10 m water depth. Values for 15 m water depth were obtained by linear interpolation.