This transformation of oceanic currents between forward and backward spinning Earths resulted from changes to
atmospheric water transport, Ziemen explained.
Not exact matches
Collision of climate variants One, called the negative phase of the Indian Ocean Dipole, is an
atmospheric circulation in the tropical Indian Ocean that
transports water from west to east.
A NOAA website on
atmospheric rivers contains this fascinating statistic that illustrates just how much moisture can be
transported by winds in the mid-to-upper atmosphere: «A strong
atmospheric river
transports an amount of
water vapor roughly equivalent to 7.5 - 15 times the average flow of liquid
water at the mouth of the Mississippi River.»
Predictive accuracies ranging from 89.4 % to as high as 99.1 % show that trained deep learning neural networks (DNNs) can identify weather fronts, tropical cyclones, and long narrow air flows that
transport water vapor from the tropics called
atmospheric rivers.
Others include poisoning of
water supplies, high levels of
atmospheric ash, crop damage, and disruption to
transport.
In GCMs, the global mean evaporation changes closely balance the precipitation change, but not locally because of changes in the
atmospheric transport of
water vapour.
This mass of warm
water, nicknamed «the Blob,» was the result of a persistent
atmospheric high - pressure ridge in the Northeastern Pacific that decreased cooling and
transport of surface
water.
A strengthening ACC created a barrier inhibiting intrusions of warm tropical
waters and minimizing both oceanic and
atmospheric heat
transport resulting in the Refrigerator Effect.
Hydrologic cycle; moisture
transport and air - ground exchange;
water budgets of meteorological phenomena; climatology of
atmospheric water
The net evaporation field (evaporation minus precipitation) shows that
atmospheric water vapor is
transported from the night side to the day side.
Associated with our work on
atmospheric circulation patterns we are studying energy
transport in the earth system and the
transport of
water in the atmosphere on different time and space scales.
The identified
atmospheric feedbacks including changes in planetary albedo, in
water vapour distribution and in meridional latent heat
transport are all poorly represented in zonal energy balance model as the one used in [7] whereas they appear to be of primary importance when focusing on ancient greenhouse climates.
So warmer - than - normal surface
waters in the South Atlantic created by the changes in
atmospheric circulation during an El Niño should be
transported northward into the North Atlantic (and vice versa for a La Niña).
Storms help replenish warm
water next to the ice, and help carry addtional heat into the melting region via
atmospheric transport of warmer moist air.
The purpose is to evaluate model ability to get the seasons right, ocean and
atmospheric transport right, hydrology and
water vapor right, and so on.
I meant this one: Makarieva, A. M., Gorshkov, V. G., and Li, B. - L.: Revisiting forest impact on
atmospheric water vapor
transport and precipitation, Theor.
The storms are being driven by an «
atmospheric river,» which, as NOAA explains, is a «relatively narrow» region in the atmosphere «responsible for most of the horizontal
transport of
water vapor outside of the tropics.»
CO2 is a «well mixed» gas in the atmosphere despite all the sources and sinks, despite the 180 ppm reading in the ice cores being too low to support C3 plants, despite the daily and seasonal sawtooth Also see former EPA scientist — slide 24: «Most of the
atmospheric carbon dioxide is being
transported by
water droplets.»
All that is needed is to add heat carried upwards past the denser atmosphere (and most CO2) by convection and the latent heat from
water changing state (the majority of heat
transport to the tropopause), the albedo effects of clouds, the inability of long wave «downwelling» (the blue balls) to warm
water that makes up 2 / 3rds of the Earth's surface, and that due to huge differences in enthalpy dry air takes far less energy to warm than humid air so temperature is not a measure of
atmospheric heat content.
I thought the idea was that an increase in the
atmospheric radiative forcing from above would warm the skin layer a bit, reducing the temp gradient to the
water layer below, thus impeding the
transport of absorbed solar energy up and back out of the ocean, and thus making it pile up to increase OHC.
The basic results of this climate model analysis are that: (1) it is increase in
atmospheric CO2 (and the other minor non-condensing greenhouse gases) that control the greenhouse warming of the climate system; (2)
water vapor and clouds are feedback effects that magnify the strength of the greenhouse effect due to the non-condensing greenhouse gases by about a factor of three; (3) the large heat capacity of the ocean and the rate of heat
transport into the ocean sets the time scale for the climate system to approach energy balance equilibrium.
This is because of the North Atlantic Current and large - scale
atmospheric circulation which
transport warm
water and air masses from lower latitudes northwards across the Atlantic and along the coast of Norway to Svalbard (Figure 1).
Depending on the conditions the clouds encounter, they can release the
atmospheric gases and in particular CO2 and
water as vapor into the atmosphere or
transport the gases to the ground in rain drops.