Not exact matches
That wind -
driven circulation
change leads to cooler
ocean temperatures on the surface of the eastern Pacific, and more heat being mixed
in and stored
in the western Pacific down to about 300 meters (984 feet) deep, said England.
Rising
temperatures and
ocean acidifi cation
drive changes in phytoplankton communities [Also see Reports by McMahon et al. and Rivero - Calle et al..]
The underlying pattern
in this year's fire forecast is
driven by the fact that the western Amazon is more heavily influence by sea surface
temperatures in the tropical Atlantic, and the eastern Amazon's fire severity risk correlates to sea surface
temperature changes in the tropical Pacific
Ocean.
They will look for evidence of
temperature changes caused by
ocean circulation patterns
in both the North Atlantic and tropical Pacific
Oceans, which
drive precipitation
in Tibet as well as the Indian monsoons.
Increased
ocean temperatures,
changes in salinity and overfishing have
driven the fish eastward.
Scientists think this reversal
in strength was
driven by
changes in sea surface
temperature and upper -
ocean ventilation.
The only time period that remotely resembles the
ocean changes happening today, based on geologic records, was 56 million years ago when carbon mysteriously doubled
in the atmosphere, global
temperatures rose by approximately six degrees and
ocean pH dropped sharply,
driving up
ocean acidity and causing a mass extinction among single - celled
ocean organisms.
Here we show that fluctuations
in Antarctic Ice Sheet discharge caused by relatively small
changes in subsurface
ocean temperature can amplify multi-centennial climate variability regionally and globally, suggesting that a dynamic Antarctic Ice Sheet may have
driven climate fluctuations during the Holocene.
Here, we elucidate this question by using 26 years of satellite data to
drive a simple physical model for estimating the
temperature response of the
ocean mixed layer to
changes in aerosol loadings.
Steric sea level is
driven by volume
changes through
ocean salinity (halosteric) and
ocean temperature (thermosteric) effects, from which the latter is known to play a dominant role
in observed contemporary rise of GSSL.
Many of the surface currents of the world
oceans (i.e., the
ocean «gyres» which appear as rotating horizontal current systems
in the upper
ocean) are
driven by the wind, however, the sinking
in the Arctic is related to the buoyancy forcing (effects that
change either the
temperature or salinity of the water, and hence its buoyancy).
If La Nina / El Nino can affect global air
temperatures in a period of a few years, than other
changes in ocean currents (
driven by AGW) can affect global atmospheric heat content
in a few years.
Small
changes in initial conditions
drive abrupt and nonlinear
change evident
in many of the global
ocean and atmospheric indices — and indeed
in the surface
temperature trajectory.
Here's a clue — a tendency toward a more frequent La Nina state,
driven specifically by increasing GH gas concentrations (and similar to conditions
in the mid-Pliocene), may provide some modulation of tropospheric
temperature spikes, but that energy will be advected somewhere (the idea of homogenous dispersion throughout the
ocean is absurd), and that somewhere is exactly where we are seeing the biggest
changes in the climate right now — the Arctic.
The issue is that differences
in mineral content, salinity, density, and
temperature all affect how the
ocean reacts to, and
drives,
changes in weather patterns, climate variations over years or decades,
ocean current circulation, etc..
Scientists think this reversal
in strength was
driven by
changes in sea surface
temperature and upper -
ocean ventilation.
Importantly, the
changes in cereal yield projected for the 2020s and 2080s are
driven by GHG - induced climate
change and likely do not fully capture interannual precipitation variability which can result
in large yield reductions during dry periods, as the IPCC (Christensen et al., 2007) states: ``... there is less confidence
in the ability of the AOGCMs (atmosphere -
ocean general circulation models) to generate interannual variability
in the SSTs (sea surface
temperatures) of the type known to affect African rainfall, as evidenced by the fact that very few AOGCMs produce droughts comparable
in magnitude to the Sahel droughts of the 1970s and 1980s.»
They also
drive the great surface
ocean currents such as the Gulf Stream: which is why ideas that these currents could stop due to
changes in water
temperature is absurd.
The arctic
temperatures and arctic ice extent varies
in a very predictable 60 - 70 year cycle that relates to
ocean cycles which are likely
driven by solar
changes.
Lamont's Ryan Abernathey and Richard Seager are studying how
changes in the
ocean cause sea surface
temperature to vary, and how these anomalies
drive changes in atmospheric circulation to create extreme weather events.
The idea is, if the
change in surface
temperature over that period is affected by
changes in cloud cover, but
changes of the surface
temperature associated with the
ocean warming are small, then
changes in cloud cover must be
driving the present global warming.
Meridional Overturning Circulation includes the action of wind, as well as density
changes through differences
in temperature and salinity
in order to
drive the
ocean currents.
Climate variability
driven by
changes in the Pacific
Ocean has affected the surface
temperature trend.
However,
in the deep tropics, where the theoretical effects on the surface energy budget of
temperature -
driven changes in evaporation and water vapour are particularly strong, there is a near quarter century record of both SST and tas from the Tropical Atmosphere
Ocean array of fixed buoys in the Pacific o
Ocean array of fixed buoys
in the Pacific
oceanocean.
Presenting such alternative figures confuses and undermines the public understanding of the actual science, which is an understanding about the
driving mechanisms of sea level rise: thermal expansion of
ocean water, melting of mountain glaciers and complex dynamics of large ice sheets —
in correspondence again with projected
temperature rise, that is
in turn a product of projected rises of greenhouse gas concentrations using calculated estimates of climate sensitivity, together creating a net disturbance
in Earth's energy balance, the very root cause of anthropogenic climate
change.
The two authors acknowledge that it is «difficult» to isolate the influence of the
ocean's effects on
temperature changes and the influence of climate - or radiation - induced
changes in driving temperature change.
Temperature changes induced by sun and
oceans drive air circulation
changes which
drive changes in every aspect of climate including convection, conduction, evaporation, condensation, precipitation, windiness, cloudiness, albedo and humidity as regards both quantities and distribution.
Like all other science, climatology is data -
driven, and the data is constantly flooding
in: measurements of
change in bird - migration patterns; details of
ocean temperatures and wind pro?les; measurements of the calcification of coral, the ripening of grapes, the retreat of glaciers, and so on.