Sentences with phrase «rate of air temperature»

I agree with your question about the impact of ice melting on reducing the rate of air temperature increases.

Just as changes in the rate of air temperature change over multi several year periods could be due to internal variability, even cessations (* which over a ten year plus period we haven't even seen) or drops in them (which we haven't seen) it's not likely.

Not exact matches

Warmer air increases the evaporation rate of water, and for every degree Celsius increase in temperature, a parcel of air can hold 7 percent more water.

If the exercise work rate is free to vary, then experimental interventions such as changes in ambient temperature, oxygen content of the inspired air, energy substrate availability or the provision of incorrect distance feedback all alter the power output (pacing strategy), whereas the rate of increase in RPE has been found to be similar between conditions.13 20 21 24 — 26

Blowing cool, dry air flowing under and through football shoulder pads reduces core body temperature and heart rate dramatically, thereby reducing the likelihood of heat illness, says a 2008 study.

Data on daily average temperature, death rates, and confounding variables (eg, humidity and air pollution) were used to calculate the temperature of minimum mortality (the optimal temperature), and to quantify total deaths due to non-optimal ambient temperature in each location.

There are some various proposed mechanisms to explain this that involve the surface energy balance (e.g., less coupling between the ground temperature and lower air temperature over land because of less potential for evaporation), and also lapse rate differences over ocean and land (see Joshi et al 2008, Climate Dynamics), as well as vegetation or cloud changes.

Assuming that their result is widely accurate wherever those can be modeled, and PR rate is proportional to the rate of ascension of air, the increase of SH due to a 0.5 C increase of surface mean temperature should be approximately 6 % of 24 W / m ^ 2 = 1.4 W / m ^ 2.

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Our modelled values are consistent with current rates of Antarctic ice loss and sea - level rise, and imply that accelerated mass loss from marine - based portions of Antarctic ice sheets may ensue when an increase in global mean air temperature of only 1.4 - 2.0 deg.

Seeing this as a baseline, positive CO2 feedback from temperature changes, or a running out of capacity for greater uptake from CO2 accumulation, would be seen as adding more CO2 to the air in addition to anthropogenic releases, but it would have to surpass some level before it would result in a total atmospheric accumulation of CO2 greater than anthropogenic emissions (first, as a rate, and later, cummulative change).

The rate and magnitude of 20th century warming are thus unknowable, and suggestions of an unprecedented trend in 20th century global air temperature are unsustainable.

Indeed, there is a clear physical reason why this is the case — the increase in water vapour as surface air temperature rises causes a change in the moist - adiabatic lapse rate (the decrease of temperature with height) such that the surface to mid-tropospheric gradient decreases with increasing temperature (i.e. it warms faster aloft).

The model variables that are evaluated against all sorts of observations and measurements range from solar radiation and precipitation rates, air and sea surface temperatures, cloud properties and distributions, winds, river runoff, ocean currents, ice cover, albedos, even the maximum soil depth reached by plant roots (seriously!).

Transient climate sensitivity: The global mean surface - air temperature achieved when atmospheric CO2 concentrations achieve a doubling over pre-industrial CO2 levels increasing at the assumed rate of one percent per year, compounded.

Temperature tends to respond so that, depending on optical properties, LW emission will tend to reduce the vertical differential heating by cooling warmer parts more than cooler parts (for the surface and atmosphere); also (not significant within the atmosphere and ocean in general, but significant at the interface betwen the surface and the air, and also significant (in part due to the small heat fluxes involved, viscosity in the crust and somewhat in the mantle (where there are thick boundary layers with superadiabatic lapse rates) and thermal conductivity of the core) in parts of the Earth's interior) temperature changes will cause conduction / diffusion of heat that partly balances the differentiTemperature tends to respond so that, depending on optical properties, LW emission will tend to reduce the vertical differential heating by cooling warmer parts more than cooler parts (for the surface and atmosphere); also (not significant within the atmosphere and ocean in general, but significant at the interface betwen the surface and the air, and also significant (in part due to the small heat fluxes involved, viscosity in the crust and somewhat in the mantle (where there are thick boundary layers with superadiabatic lapse rates) and thermal conductivity of the core) in parts of the Earth's interior) temperature changes will cause conduction / diffusion of heat that partly balances the differentitemperature changes will cause conduction / diffusion of heat that partly balances the differential heating.

My guess on why was shown at RC a few weeks ago in comment # 12... Wayne, if it's true as you indicated in 9, that upper air temperatures are increasing at a much stronger rate than near the surface, it seems to me the departure would explain at least part of what seems to be a large increase in world area having minimal rainfall and drought... at: http://www.realclimate.org/index.php/archives/2006/07/peter-doran-and-how-misleading-talking-points-propagate/

Predicting sea ice extent is easy if you can mentally calculate wind variations, momentum, sea currents, multi year ice compression ratios, tidal synergy with weather patterns, the AO, the temperature of ice sea water and air, how cloudy it will be, salinity, pycnocline convection rates, sea surface to air interface, CO2 exchange, ice thickness distributions.....

While 2009 showed a slowdown in the rate of annual air temperature increases in the Arctic, the first half of 2010 shows a near record pace with monthly anomalies of over 4 °C in northern Canada.

«Even if an area remains wet doesn't mean that it will be protected from the other aspects of climate change: rising and far more erratic air temperatures, higher rates of evaporation (evapotranspiration), and the rising concentration of CO2,» he said in an e-mail message.

Similar negative effects occur with worsening air pollution — higher levels of ground - level ozone smog and other pollutants that increase with warmer temperatures have been directly linked with increased rates of respiratory and cardiovascular disease — food production and safety — warmer temperatures and varying rainfall patterns mess up staple crop yields and aid the migration and breeding of pests that can devastate crops — flooding — as rising sea levels make coastal areas and densely - populated river deltas more susceptible to storm surges and flooding that result from severe weather — and wildfires, which can be ancillary to increased heat waves and are also responsible for poor air quality (not to mention burning people's homes and crops).

Although the rate of warming of surface air and lower troposphere temperatures appear to have slowed over the past few years, the same could be said at any virtually any point in time by cherrypicking short - term noise and ignoring the long - term trend (Figure 2).

However, if the air continues to cool below freezing point then, although the nett flow of heat from the water is greater while the water is in the process of freezing, the air temperature does not rise and will continue to tend to fall, albeit at a slower rate.

c) If the If the rate of heat loss from the air was about the same as the rate of heat gain from the water, then its temperature would stay almost the same, and it would warm up when the water started freezing.

Peter, You are exactly correct.Up until: Depending on the rate at which the air is cooling, it will either mean that the rate of cooling of the air slows down, or the air temperature remains the same.

Whereas the CO2 has reduced the rate of uplift in the ascending column (which warms the surface) CO2 at lower levels reduces the rate of descent in the descending column which reduces surface temperature because less warmth is then being generated via compression of descending air.

However, despite near normal rates of ice loss during the month, June 2015 was a relatively warm month (Figure 7) with 925 hPa air temperatures up to 2.5 C higher than average near the North Pole and East Siberian Sea, with even warmer air temperatures in the Kara Sea (up to 4.5 C).

If the air temperature starts rising then the rate of heat flow from the water to the air slows down and the water consequently stops freezing, so the latent energy falls and so the temperature tends to stabilize at that point.

The parcel of air changes its own temperature and pressure at the same rate as the temperature and pressure of the surroundings changes.

Furthermore one third of the non passive house designs were not balanced, which would affect flow rates in different rooms, the efficiency of the heat recovery, and, therefore the temperature of the supply air (this is not covered in part F).

Heat (not latent heat) is removed prior to condensation by conversion of kinetic energy to potential energy which then provokes condensation and when the phase change occurs the release of latent heat causes the air parcel to rise a little further with additional conversion of KE to PE until it reaches the correct lapse rate temperature for its height and then it stops rising and begins to descend.

I left that for JIM D, but the rate of warming of the surface air decreases as the ocean temperature increases.

Many retreats began with an increase in thinning rates near the front in the summer of 2003, a year of record high coastal - air and sea - surface temperatures.

What Willis is describing is that vulcanism can effect air temperature and clouds, the changed air temperature subtly changes the diurnal timing of cloud formation and that changes the rate of thermal charge accumulating in the oceans which ultimately is discharged in an El Niño.

A slight reduction in the rate of transfer from ocean to air courtesy of more IR returned from the air is sufficient to force a higher surface temperature.

Comparison of ablation rates and onsite temperature records in the case of the South Cascade Glacier, Easton Glacier, Ice Worm Glacier and Columbia Glacier yield a relationship between air temperature and daily ablation for snow and ice in SWE (Figure 1).

Sealing time of air bubbles at best about 70 years and mixing with ambient air through diffusion all that time, chemical changes thereafter, different diffusion rates for different gases thereafter... ice cores are a target - rich environment for casting of doubt about how well they perform as global temperature proxies.

Arctic air temperatures are increasing at twice the rate of the rest of the world — a study by the U. S. Navy says that the Arctic could lose its summer sea ice by next year, eighty - four years ahead of the models — and evidence little more than a year old suggests the West Antarctic Ice Sheet is doomed, which will add between twenty and twenty - five feet to ocean levels.

The average position of the ITCZ is situated north of the equator because most ocean is in the southern hemisphere and it is ocean temperatures that dictate its position by governing the rate of energy transfer from oceans to air.

This is based on Schurer's 5th - 95th percentile range of current warming relative to the late - 1800s, using the Cowtan and Way temperature record corrected for the difference between sea surface temperature and surface air temperature warming rates.

From an OSU press release: CORVALLIS, Ore. — An analysis of 35 headwater basins in the United States and Canada found that the impact of warmer air temperatures on streamflow rates was less than expected in many locations, suggesting that some ecosystems may be resilient to certain aspects of climate change.

The resulting enhanced loss of summer and winter sea ice resulted in feedbacks, associated with Arctic Amplification, which has raised Arctic air temperatures at a rate twice the global average.

If the air is dry and the process is adiabatic, the rate of temperature fall is 1 °C per 100 meters of lift.

1) The differential form of Henry's Law says that the diffusion rate of a gas from water into the air is a function only of the concentration of the gas in the water (given the diffustion coefficient, which is constant for a constant temperature).