Sensitivity experiments show that atmospheric CO2 closely follows decadal - mean temperature changes
when changes in ocean circulation and ocean - sediment interactions are not important.
Not exact matches
The goal is to capture natural variations
in the climate, like
changes in ocean circulation or features like the El Niño Southern Oscillation, that are swamped by the signal of human - caused warming
when looking out to the end of the century.
In the paper Gray makes many extravagant claims about how supposed changes in the THC accounted for various 20th century climate changes («I judge our present global ocean circulation conditions to be similar to that of the period of the early 1940s when the globe had shown great warming since 1910, and there was concern as to whether this 1910 - 1940 global warming would continu
In the paper Gray makes many extravagant claims about how supposed
changes in the THC accounted for various 20th century climate changes («I judge our present global ocean circulation conditions to be similar to that of the period of the early 1940s when the globe had shown great warming since 1910, and there was concern as to whether this 1910 - 1940 global warming would continu
in the THC accounted for various 20th century climate
changes («I judge our present global
ocean circulation conditions to be similar to that of the period of the early 1940s
when the globe had shown great warming since 1910, and there was concern as to whether this 1910 - 1940 global warming would continue.
You've got the radiative physics, the measurements of
ocean temperature and land temperature, the
changes in ocean heat content (Hint — upwards, whereas if if was just a matter of
circulation moving heat around you might expect something more simple) and of course observed predictions such as stratospheric cooling which you don't get
when warming occurs from oceanic
circulation.
The paleoclimate record (8.2 kyr, and earlier «large lake collapses») shows a dramatic drop
in surface temperatures for a substantial period of time
when the
ocean circulation shuts off or
changes, but is that actually what would be expected under these warming conditions?
For weather predictions, accuracy disappears within a few weeks — but for
ocean forecasts, accuracy seems to have decadal scale accuracy — and
when you go to climate forcing effects, the timescale moves toward centuries, with the big uncertainties being ice sheet dynamics,
changes in ocean circulation and the biosphere response.
This thesis presents the results of several general
circulation model simulations aimed at studying the effect of
ocean circulation changes when they occur
in conjunction with increased atmospheric trace gas concentrations.
The new study explores what happened to
ocean circulation when the Earth went through a series of abrupt climate
changes in the past, during a time
when ice covered part of North America and temperatures were colder than today.
The most likely candidate for that climatic variable force that comes to mind is solar variability (because I can think of no other force that can
change or reverse
in a different trend often enough, and quick enough to account for the historical climatic record) and the primary and secondary effects associated with this solar variability which I feel are a significant player
in glacial / inter-glacial cycles, counter climatic trends
when taken into consideration with these factors which are, land /
ocean arrangements, mean land elevation, mean magnetic field strength of the earth (magnetic excursions), the mean state of the climate (average global temperature), the initial state of the earth's climate (how close to interglacial - glacial threshold condition it is) the state of random terrestrial (violent volcanic eruption, or a random atmospheric
circulation / oceanic pattern that feeds upon itself possibly) / extra terrestrial events (super-nova
in vicinity of earth or a random impact) along with Milankovitch Cycles.
When a full - depth
ocean model is used, something intriguing happens: the loss of Arctic sea ice triggers a far - flung response that mimics climate
change itself, including a slowdown of the Atlantic Meridional Overturning
Circulation (AMOC), a build - up of heat
in the tropical
oceans over several decades, and a warming of the atmosphere a few miles above the tropics.