«The study demonstrates a robust century - scale link
between ocean circulation changes in the Atlantic basin and rainfall in the adjacent continents during the past 4,000 years,» said UTIG Director Terry Quinn, a co-author on the study.
Not exact matches
The main feedbacks
between climate and the ice sheet arise from
changes in ice elevation, atmospheric and
ocean circulation, and sea - ice distribution.
Climate and
ocean -
circulation changes that happened millions of years ago likely contributed to the differences in appearance
between certain species of male and female seals.
There is a potential for both positive and negative feedbacks
between the
ocean and atmosphere, including
changes in both the physics (e.g.,
circulation, stratification) and biology (e.g., export production, calcification) of the
ocean.
What if the mixing
between the
oceans were drastically reduced due to
changes in
ocean circulation?
Everything else that might try to alter that base level simply results in atmospheric
circulation changes (atmosphere includes
oceans for this purpose) that adjust the rate of conversion
between kinetic and potential energy so as to keep the base level of system energy content stable.
Here a simple biologically and physically - based model of sapflow potential is used to assess observed
changes in sapflow across the Northeastern US from 1980 to 2006; document the correspondence
between these observations and independent downscaled atmosphere
ocean general
circulation model (AOGCM) simulations of conditions during this period; and quantify
changes in sapflow potential through 2100.
Climate and
ocean -
circulation changes that happened millions of years ago likely contributed to the differences in appearance
between certain species of male and female seals.
There seems to be some sort of interaction
between the air
circulation and the
ocean circulation which
changes depending on whether the
oceans are globally warming the air or globally cooling it.
«The authors write that North Pacific Decadal Variability (NPDV) «is a key component in predictability studies of both regional and global climate
change,»... they emphasize that given the links
between both the PDO and the NPGO with global climate, the accurate characterization and the degree of predictability of these two modes in coupled climate models is an important «open question in climate dynamics» that needs to be addressed... report that model - derived «temporal and spatial statistics of the North Pacific
Ocean modes exhibit significant discrepancies from observations in their twentieth - century climate... conclude that «for implications on future climate
change, the coupled climate models show no consensus on projected future
changes in frequency of either the first or second leading pattern of North Pacific SST anomalies,» and they say that «the lack of a consensus in
changes in either mode also affects confidence in projected
changes in the overlying atmospheric
circulation.»»
«The situation is important for us, as the reduced temperature gradient
between the equator and the North Pole is
changing the
circulation patterns and behaviours of the atmosphere and
oceans, contributing to our direct experience of climate disruption.»
Between its Second and Third Assessment Reports, the Intergovernmental Panel on Climate
Change elaborated long - term greenhouse gas emissions scenarios, in part to drive global ocean - atmosphere general circulation models, and ultimately to assess the urgency of action to prevent the risk of climatic c
Change elaborated long - term greenhouse gas emissions scenarios, in part to drive global
ocean - atmosphere general
circulation models, and ultimately to assess the urgency of action to prevent the risk of climatic
changechange.
This major
change in
ocean circulation, along with a climate that had already been slowly cooling for millions of years, may be what led to ice accumulation most of the time — but also to climatic instability, with flips every few thousand years or so
between warm - and - wet and cool - and - dry.
As sub-surface oxygen concentrations in the
ocean everywhere reflect a balance
between supply through
circulation and ventilation and consumption by respiratory processes, the absolute amount of oxygen in a given location is therefore very sensitive to
changes in either process, more sensitive perhaps as other physical and chemical parameters.
The seasonal climate may relate to
changes in the
ocean circulation pattern prior to 4.6 Ma that resulted in an increased temperature and atmospheric pressure gradient between the east coast of North America and the Atlantic Ocean, but this climate phase seems to be only a temporary condition, as underlying and overlying sediment are both consistent with drier condit
ocean circulation pattern prior to 4.6 Ma that resulted in an increased temperature and atmospheric pressure gradient
between the east coast of North America and the Atlantic
Ocean, but this climate phase seems to be only a temporary condition, as underlying and overlying sediment are both consistent with drier condit
Ocean, but this climate phase seems to be only a temporary condition, as underlying and overlying sediment are both consistent with drier conditions.
The dust - induced thermal contrast
changes between the Eurasian continent and the surrounding
oceans are found to trigger or modulate a rapidly varying or unstable Asian winter monsoon
circulation, with a feedback to reduce the dust emission from its sources (Zhang et al., 2002).
In addition, the authors provide compelling evidence of both the important coupling of
ocean and atmosphere processes and the strong communication, of effects of climatic
change,
between the waters of the Northern and Southern hemisphere through global
ocean circulation.»
Irrigation effects on climate may also be indirect, especially in monsoon regions where alteration of the thermal contrast
between land and
ocean may produce
changes in monsoon
circulation and the accompanying climatic variables.