That property of water could be enough to enable the weather processes overall to stabilise the whole process and is one of the reasons why oceanic temperature is, always has been and always will be the primary
atmospheric temperature driver and will always reduce or possibly neutralise any effect of an enhanced greenhouse effect in the absence of really huge changes caused by astronomic or geological processes.
Not exact matches
The relative
atmospheric concentrations of greenhouse gases as well as aerosol and particulate content coupled with other climate information gives insight into both the importance of these as
drivers of
temperature as well as how these
drivers might couple in either a positive or negative feedback sense (Beckman and Mahoney, 1998).
The assessment considered the impacts of several key
drivers of climate change: sea level change; alterations in precipitation patterns and subsequent delivery of freshwater, nutrients, and sediment; increased ocean
temperature; alterations in circulation patterns; changes in frequency and intensity of coastal storms; and increased levels of
atmospheric CO2.
Although the primary
driver of glacial — interglacial cycles lies in the seasonal and latitudinal distribution of incoming solar energy driven by changes in the geometry of the Earth's orbit around the Sun («orbital forcing»), reconstructions and simulations together show that the full magnitude of glacial — interglacial
temperature and ice volume changes can not be explained without accounting for changes in
atmospheric CO2 content and the associated climate feedbacks.
As that happens, the underlying global warming
driver will be progressively loosing its energy sink, and not only will we see ocean rise, but a progressive escalation in the rate of
atmospheric temperature rise as well.
The CO2 concentration is a primary
driver of
atmospheric and surface
temperature.
Here we analyze a series of climate model experiments along with observational data to show that the recent warming trend in Atlantic sea surface
temperature and the corresponding trans - basin displacements of the main
atmospheric pressure centers were key
drivers of the observed Walker circulation intensification, eastern Pacific cooling, North American rainfall trends and western Pacific sea - level rise.
«We also present a set of global vulnerability
drivers that are known with high confidence: (1) droughts eventually occur everywhere; (2) warming produces hotter droughts; (3)
atmospheric moisture demand increases nonlinearly with
temperature during drought; (4) mortality can occur faster in hotter drought, consistent with fundamental physiology; (5) shorter droughts occur more frequently than longer droughts and can become lethal under warming, increasing the frequency of lethal drought nonlinearly; and (6) mortality happens rapidly relative to growth intervals needed for forest recovery.
A recent study found that «almost two - thirds of the impacts related to
atmospheric and ocean
temperature can be confidently attributed to anthropogenic forcing» (meaning human caused
drivers).
At present,
atmospheric temperature is decreasing and CO2 is increasing again showing that CO2 is not the principal
driver of climate change.
One
driver of this is anomalies in sea surface
temperature which effect large scale
atmospheric circulation and, in turn, influence precipitation.
«Whilst there are certainly other potential
drivers of changes in the climate we know that over the last century we have greatly increased the CO2 concentration in the atmosphere and, through detection and attribution analyses, we know that the rising levels of
atmospheric CO2 and other greenhouse gases have driven the rise in global
temperature,» King said.
The relative
atmospheric concentrations of greenhouse gases as well as aerosol and particulate content coupled with other climate information gives insight into both the importance of these as
drivers of
temperature as well as how these
drivers might couple in either a positive or negative feedback sense.
The relative
atmospheric concentrations of greenhouse gases as well as aerosol and particulate content coupled with other climate information gives insight into both the importance of these as
drivers of
temperature as well as how these
drivers might couple in either a positive or negative feedback sense (Beckman and Mahoney, 1998).
Such oscillations might also alter hurricane patterns, but the main
driver of hurricanes is warm sea surface
temperatures > 27C (we can all agree on that, I hope);
atmospheric conditions also need to be conducive (see the above comment on this year's rip - snorting season).
Global data on anthropogenic aerosols is poor to non-existent, but I would content that reductions in aerosols were a significant
driver of low level cloud decreases over the 1975 to 2000 period, and hence
atmospheric temperatures.