Frontiers in Decadal Climate Variability Proceedings of a Workshop (2016) / Chapter Skim
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The Role of External Forcing
The Role of External Forcing
Pages 31-34
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From page 31... ...
If one considers oce warming as a proxy for radiation imb ean a r balance, then the continnued warming suggests that the amount of radiative im g t o mbalance at th top of the he atmosphere may have remained unchanged betwe the 1990s and the 200 r een s 00s, arguing against a significant effe of changes in external fo s ect s orcings on GMMST. Susan Solo omon from the Massachuse Institute of Technology provided a brief survey of etts radiative forcing changes during 200 f 00-2014 that might have co m ontributed to t decadal the rates of glo obal surface warming.
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From page 32... ...
The ash degree) of tropical SSTs after the Nabro particles from the eruptions tend to be volcanic eruption in 2011 suggests a forced large enough to fall out quickly, but the component to observed tropical sea surface sulfurous gases form highly reflective temperature (SST)
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From page 33... ...
, stratosphe water vapo significantly d eric or dropped and sta ayed low through much of the 2000s. SOURC Solomon et al.
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