In the central United States, for example, observational data indicate that rainfall increased, surface air temperature decreased, and
surface humidity increased during the summer over the course of the 20th century concurrently with increases in both agricultural production and global GHG emissions.
Not exact matches
And a third found that climate - induced sea -
surface temperature anomalies over the northeast Pacific were driving storms (and moisture) away from California, but the warming also caused
increased humidity — two competing factors that may produce no net effect.
Surface specific
humidity has generally
increased after 1976 in close association with higher temperatures over both land and ocean.
A compilation of
surface measurements of downward longwave radiation from 1973 to 2008 find an
increasing trend of more longwave radiation returning to earth, attributed to
increases in air temperature,
humidity and atmospheric carbon dioxide (Wang 2009).
The layer will also gradually
increase its
humidity by evaporation of the ocean or lake
surface, as well as by the effect of cooling itself.
First of all it is important to note that even pure greenhouse gas forcing will lead to a slight decrease in
surface solar radiation (due to the concurrent
increased humidity) and potential cloud feedbacks.
Now since relative
humidity remains roughly constant at the ocean
surface and the air's capacity to hold water
increases with temperature, relative
humidity will actually decrease over land, particularly as one enters the continental interiors.
CO2's effect of stimulating plant growth and
increasing plant tolerance of aridity contributed to revegetating large areas of land that were desert at the LGM, compounding the effects of an
increase in atmospheric
humidity, reduced land / ocean
surface ocean ration, and
increased warmth, all of which combined caused the reduction of airborne dust and atmosperic albedo.
There will be Regionally / locally and temporal variations;
increased temperature and backradiation tend to reduce the diurnal temperature cycle on land, though regional variations in cloud feedbacks and water vapor could cause some regions to have the opposite effect; changes in
surface moisture and
humidity also changes the amount of convective cooling that can occur for the same temperature distribution.
The 2009 State of the Climate Report of the US National Oceanic and Atmospheric Administration (NOAA) tells us that climate change is real because of rising
surface air temperatures since 1880 over land and the ocean, ocean acidification, sea level rise, glaciers melting, rising specific
humidity, ocean heat content
increasing, sea ice retreating, glaciers diminishing, Northern Hemisphere snow cover decreasing, and so many other lines of evidence.
Even in areas where precipitation does not decrease, these
increases in
surface evaporation and loss of water from plants lead to more rapid drying of soils if the effects of higher temperatures are not offset by other changes (such as reduced wind speed or
increased humidity).5 As soil dries out, a larger proportion of the incoming heat from the sun goes into heating the soil and adjacent air rather than evaporating its moisture, resulting in hotter summers under drier climatic conditions.6
Evaporation
increases with rising
surface temperature, decreasing relative
humidity, and
increasing surface wind speed.
Surface measurements of downward longwave radiation A compilation of surface measurements of downward longwave radiation from 1973 to 2008 find an increasing trend of more longwave radiation returning to earth, attributed to increases in air temperature, humidity and atmospheric carbon dioxide (Wang
Surface measurements of downward longwave radiation A compilation of
surface measurements of downward longwave radiation from 1973 to 2008 find an increasing trend of more longwave radiation returning to earth, attributed to increases in air temperature, humidity and atmospheric carbon dioxide (Wang
surface measurements of downward longwave radiation from 1973 to 2008 find an
increasing trend of more longwave radiation returning to earth, attributed to
increases in air temperature,
humidity and atmospheric carbon dioxide (Wang 2009).
Increasing the
surface temperature over the ocean by 1 °C should
increase the
humidity of saturation and thus the absolute
humidity by 8 percent.
A compilation of
surface measurements of downward longwave radiation from 1973 to 2008 find an
increasing trend of more longwave radiation returning to earth, attributed to
increases in air temperature,
humidity and atmospheric carbon dioxide (Wang 2009).
But, just in case you were semi-serious: With oceans covering 70 % of the earth's
surface, you could never change atmospheric
humidity — water vapor pressure is a function of atmospheric temperature,
increasing as temperature rises.
Sufficient glacial expansion will reduce lower atmospheric
humidity, reduce kinetic induction within the lower atmosphere and hence
increase the «thermal gap» tween lower atmosphere and
Surface.
«Trends in U.S.
Surface Humidity, 1930 — 2010 -LSB-...]
Increasing evidence from observations and climate models indicates that anthropogenic activity is increasing atmospheric moisture (Boucher et al. 2004; Willett et al. 2007; Santer et al. 2007; Min et
Increasing evidence from observations and climate models indicates that anthropogenic activity is
increasing atmospheric moisture (Boucher et al. 2004; Willett et al. 2007; Santer et al. 2007; Min et
increasing atmospheric moisture (Boucher et al. 2004; Willett et al. 2007; Santer et al. 2007; Min et al. 2008).
The
increase in relative
humidity is due to warmer
surface sea temperatures allowing greater evaporation and warmer polar conditions causing less condensation.
WebHubTelescope Bottom line is that the
SURFACE specific
humidity increased while the relative
humidity decreased.
Typically, the risk of
surface condensation and mould growth
increases with internal
humidity loads in buildings and / or reduced quality of the thermal envelope.
Air in clouds and immediately next to the ocean
surface is at or near 100 % relative
humidity, so as temperatures
increase the absolute
humidity there also
increases.
Is this point only about the radiative characteristics of the H2O vapour, and the assumption that relative and / or specific
humidity should rise thanks to CO2 - induced
increased evaporation, which in turn would
increase downwelling heat radiation — or just the part that slightly hotter
surface (due to CO2) also emits more heat to be trapped by the vater vapour?
The average absolute
humidity also
increases between the clouds and the ocean
surface with
increasing temperatures.
Increasing humidity decreases the lapse rate (lapse rate feedback), allowing the upper atmosphere to warm more rapidly than the
surface and more OLR to escape for a given rise in
surface temperature.
It has
increased the
humidity of the atmosphere, altered the atmospheric vertical motion and associated cloud fields, and perturbed the longwave and shortwave radiative fluxes at the continental
surface.
Therefore, assuming that the relative
humidity remains about constant, the strength of the greenhouse effect will
increase with
surface temperature.
That is what happens when oceans naturally
increase their emission of energy and the response of the air is exactly the same whether the warmer ocean
surface is a result of enhanced energy emission from the ocean or enhanced energy in the air from another cause such as more
humidity or more CO2.
That mechanism is missing in the GCMs, which
increase specific
humidity with
surface temperature but keep cloud cover parameterized and constant.
Over the ocean, the observed
surface specific
humidity increases at 5.7 % per 1ºC warming, which is consistent with a constant relative
humidity.
Climate models (for various obscure reasons) tend to maintain constant relative
humidity at each atmospheric level, and therefore have an
increasing absolute
humidity at each level as the
surface and atmospheric temperatures
increase.
Philipona et al. (2004) measured the changes and trends of radiative fluxes at the
surface and their relation to greenhouse gas increases and temperature and humidity changes measured from 1995 to 2002 at eight stations of the Alpine Surface Radiation Budget (ASRB) n
surface and their relation to greenhouse gas
increases and temperature and
humidity changes measured from 1995 to 2002 at eight stations of the Alpine
Surface Radiation Budget (ASRB) n
Surface Radiation Budget (ASRB) network.
The relative
humidity increases as the
surface temperature goes down, so it is directly related to the window staying warm.
During a dry winter, the reduction of aerosol concentrations in weekend days may overwhelmingly impact on the DTR through a direct effect, i.e. by
increasing total solar irradiance near the
surface and raising the daytime temperature and maximum temperature, and lowering relative
humidity.
In the lower atmosphere, the available data points to
increasing water vapor content, but because of large variations in local
humidity from day to night, from day to day, and from season to season, no - one currently knows exactly how much more water vapor is going into the air (IPCC Working Group 1 Assessment Report 4, Chapter 3, «Observations:
Surface and Atmospheric Climate Change», page 273).
And yes, greenhouse warming could be due to
increased humidity, which in turn could be due to normal variability in the ocean
surface temperature.
Eventually the
surface will cool sufficiently to produce an observed reversion of the warming trend that
increased the level of «
humidity».
According to Isaac Held, climate models predict that the relative
humidity over oceans will have to rise about 1 % (a 5 %
increase in 1 — RH) to suppress
surface evaporation which would otherwise rise at 7 % / degC and create a
surface energy imbalance (because DLR
increases with warming nearly as fast as OLR).
One study, published in today's edition of the journal Nature, found that the overall
increase in worldwide
surface humidity from 1973 - 99 was 2.2 %, which is due «primarily to human - caused global warming,» according to study co-author Nathan Gillett of the University of East Anglia, in Norwich, U.K.
Irrigation also leads to boreal winter (December - February) warming over parts of North America and Asia in the latter part of the century, due to enhanced downward longwave fluxes from
increased near
surface humidity.