In Zhang et al. (2013), Fig. 3 was processed incorrectly and the land values in panel (b) were mistakenly omitted. The figure appears below as it was meant to appear originally.

Fig. 3.

Climatological mean during the boreal cold seasons (November–April) between 60°S and 60°N for (a) stratiform cloud amount (%, period: 1984–2007), (b) water cloud amount (%, period: 1982–2007), and (c),(d) SWCF and NCRF, respectively (W m−2, period: 2001–10).

Fig. 3.

Climatological mean during the boreal cold seasons (November–April) between 60°S and 60°N for (a) stratiform cloud amount (%, period: 1984–2007), (b) water cloud amount (%, period: 1982–2007), and (c),(d) SWCF and NCRF, respectively (W m−2, period: 2001–10).

The staff of the Journal of Climate regrets any inconvenience this error may have caused.

REFERENCE

REFERENCE
Zhang
,
Y.
,
R.
Yu
,
J.
Li
,
W.
Yuan
, and
M.
Zhang
,
2013
:
Dynamic and thermodynamic relations of distinctive stratus clouds on the lee side of the Tibetan Plateau in the cold season
. J. Climate,
26
,
8378
8391
, doi:.