The Version 5.6 global average lower tropospheric temperature (LT) anomaly for November, 2014 is +0.33 deg. C, down a little from the October value of +0.37 deg. C (click for full size version):

The global, hemispheric, and tropical LT anomalies from the 30-year (1981-2010) average for the last 23 months are:
    YR  MON  GLOBAL   NH    SH    TROPICS
    2013    1   +0.497   +0.517   +0.478   +0.386
    2013    2   +0.203   +0.372   +0.033   +0.195
    2013    3   +0.200   +0.333   +0.067   +0.243
    2013    4   +0.114   +0.128   +0.101   +0.165
    2013    5   +0.082   +0.180  -0.015   +0.112
    2013    6   +0.295   +0.335   +0.255   +0.220
    2013    7   +0.173   +0.134   +0.211   +0.074
    2013    8   +0.158   +0.111   +0.206   +0.009
    2013    9   +0.365   +0.339   +0.390   +0.190
    2013   10   +0.290   +0.331   +0.249   +0.031
    2013   11   +0.193   +0.160   +0.226   +0.020
    2013   12   +0.266   +0.272   +0.260   +0.057
    2014    1   +0.291   +0.387   +0.194  -0.029
    2014    2   +0.170   +0.320   +0.020  -0.103
    2014    3   +0.170   +0.338   +0.002  -0.001
    2014    4   +0.190   +0.358   +0.022   +0.092
    2014    5   +0.326   +0.325   +0.328   +0.175
    2014    6   +0.305   +0.315   +0.295   +0.510
    2014    7   +0.304   +0.289   +0.319   +0.451
    2014    8   +0.199   +0.244   +0.153   +0.061
    2014    9   +0.294   +0.187   +0.401   +0.181
    2014   10   +0.365   +0.333   +0.396   +0.189
    2014   11   +0.329   +0.356   +0.302   +0.252
As I have mentioned before, month-to-month variations in global tropospheric temperature can be rather large just due to variations in convective overturning of the atmosphere (storm activity). To demonstrate how large the changes can be, the following plot shows the daily temperature anomalies for November, 2014. Note that the tropical troposphere warmed by 0.5 deg. C in less than 2 weeks, presumably coming out of a less convective phase.
Despite this rise in late November tropical temperatures, note the extratropics must have cooled since both the NH and SH show downward trends. While this variability in tropospheric temperature might suggest just how dynamic the climate system is, it requires less than 10% variability in storm activity. In general, rapid tropospheric warming events occur during SST cooling (and vice versa), which is much weaker in magnitude owing to the very different heat capacities of water versus air.
The global image for November should be available in the next day or so here.
Popular monthly data files (these might take a few days to update):
uahncdc_lt_5.6.txt (Lower Troposphere)
uahncdc_mt_5.6.txt (Mid-Troposphere)
uahncdc_ls_5.6.txt (Lower Stratosphere)

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