Also, don't forget the «SO» part of the El Niño / Southern Oscillation (ENSO), which is the all -
important atmospheric response.
Not exact matches
Since El Nino also has an
important impact on the Asian Summer Monsoon in particular, its hard to know precisely what large - scale changes in
atmospheric circulation are due to the radiative forcing of the eruption itself, and the secondary
response to that eruption of ENSO.
One recent study, for example, presented a thorough and careful scrutiny of hundreds of peer - reviewed scientific publications evaluating the accuracy and capability of climate models to simulate the
response of a number of
important climatic phenomena to rising
atmospheric CO2 concentrations.
Methane is an
important part of the anthropogenic radiative forcing Methane emissions have a direct GHG effect, and they effect
atmospheric chemistry and stratospheric water vapour which have additional impacts natural feedbacks involving methane likely to be
important in future — via wetland
response to temperature / rain change,
atmospheric chemistry and, yes, arctic sources There are large stores of carbon in the Arctic, some stored as hydrates, some potentially convertible to CH4 by anaerobic resporation [from wikianswers: Without oxygen.
But the
important problem for modern climate science is to predict and to measure the
response of other
atmospheric variables (temperature, humidity and cloud) to a climate forcing.
Based on the understanding of both the physical processes that control key climate feedbacks (see Section 8.6.3), and also the origin of inter-model differences in the simulation of feedbacks (see Section 8.6.2), the following climate characteristics appear to be particularly
important: (i) for the water vapour and lapse rate feedbacks, the
response of upper - tropospheric RH and lapse rate to interannual or decadal changes in climate; (ii) for cloud feedbacks, the
response of boundary - layer clouds and anvil clouds to a change in surface or
atmospheric conditions and the change in cloud radiative properties associated with a change in extratropical synoptic weather systems; (iii) for snow albedo feedbacks, the relationship between surface air temperature and snow melt over northern land areas during spring and (iv) for sea ice feedbacks, the simulation of sea ice thickness.
If the acidification event occurred in this manner it has
important implications for how strongly the Earth might warm in
response to increases in
atmospheric CO2.
[
Response: Isaac, I don't think anyone is claiming that SSTs alone are determinant (since as you correctly point out, tropospheric temperatures and the stability of the
atmospheric profile are obviously
important).
OCO - 2 observations confirm that the tropical Pacific Ocean played an early and
important role in the
response of
atmospheric CO2 concentrations to the 2015 — 2016 El Niño.