Sentences with phrase «atmosphere during»

Not only does it look great but it creates a cosy atmosphere during the winter months.

«It is also nice to spend time with members in a more relaxed atmosphere during scheduled pre-meeting activities; noting recent tours of The Clare and The Admiral, two newly constructed high - rise CCRCs in Chicago were arranged.

I can picture the tremendous atmosphere during a real estate convention.

Divorce Source provides people with the opportunity to meet people online in a supportive atmosphere during what is an utmost difficult time.

Erla aims to create a comfortable atmosphere during her sessions and puts a great emphasis on monitoring the progress and outcome of therapy to ensure that therapy is benefiting her clients and serving their best interests.

• Worked with office administration in the processing of new business and inspired an efficient and productive office atmosphere during high pressure points of the year.

Build positive atmosphere during tests aimed at reducing stress and encouraging success.

We expect that some fraction of the NF3 produced will escape to the atmosphere during production, transport, use, or disposal.

Finally, the Escape will be easier on L.A.'s notoriously bad smog: according to one Ford sales manager,» [the Escape Hybrid] releases fewer smog - forming emissions into the atmosphere during a three - hour drive (about 180 miles) than grilling one hamburger in your back yard.»

Another brainstorm suggests that by creating «biochar» we can arrest the amount of carbon dioxide that naturally goes into the atmosphere during plant decay.

As Gore notes, scientists have observed a pattern of steadily increasing concentrations of CO2 in the atmosphere during the past half - century.

However I have some doubts: 1) You explained how tree rings may be used to determine the concentration of CO2 in the atmosphere during the tree lives.

For instance the recordbreaking yearly increase of anthropogenic CO2 emissions to atmosphere during 2010 has been 6 %; from total anthropogenic CO2 emissions of about 8 Gt a year (calculated in carbon) that 6 % makes about 0.5 Gt CO2 a year.

The CO2 removed from the atmosphere during the plant's growth is then «locked in» to the soil.

The ocean loses the heat stored from the summer into the atmosphere during winter.

Warmer and significantly larger ocean surfaces also allow considerably more CO2 to evaporate into the atmosphere during warm periods (your soda pop after it is exposed for an hour goes flat — same principle).

036 °C / yr and leaving an energy of 14.8 to 18.4 1019 J / yr available; (2) the increase of the atmosphere - related ice melt between these two periods amounts to 316 Gt / yr which requires 10.5 1019 J / yr, i.e. between 57 % and 71 % of the energy left by the slowdown; and (3) the energy budget shows therefore that the heat required to melt this additional 316 Gt / yr of ice is of the same order as the energy needed to warm the atmosphere during the decade 2002 — 2011 as much as during the previous one, suggesting a redistribution of heat within the atmosphere - cryosphere system.

Emissions from burning these fuels total nearly two - thirds of all the carbon that has been emitted into the atmosphere during the industrial era.

However, less of these other pollutants are released into the atmosphere during modern fossil fuel combustion.

So isn't the whole issue really revolving around how dense the atmosphere is at any given time and has atmosphere during the latest warm spell been denser than say in the 1970s during that cold spell?

So during a high pressure, distant objects (mountains etc) appear more distant, with less visible definition to the details, and appear closer with greater visible detail pre a change in the weather (its very noticeable)... Is this the result of the SW light being scattered / or absorbed by the greater density o water molecules in the atmosphere during a high pressure system?

For instance all the increase of CO2 in the atmosphere during the industrial time, without any proper evidence in reality, is assumed to be anthropogenic.

There is no strong direct relationship between the human caused emissions of a single year and the uptake from the atmosphere during the same year.

Therefore, the contention that the ocean does not (did not) release heat into the atmosphere during the 1970 - 2000 can not be true and therefore the statement that all of the observed warming during that time period was due to human causes incorrect.

Even on the Siberian continental margin, where water temperatures are colder than the global average, and where the sediment column retains the cold imprint from its exposure to the atmosphere during the last glacial time 20,000 years ago, any methane hydrate must be buried under at least 200 m of water or sediment.

When you say «we're» cooling now, you must mean the troposphere over some short period of time and certianly less heat is flowing from ocean to atmosphere during the current cool PDO.

An unknown amount of methane is lost into the atmosphere during fracking, extraction, transport and distribution.

Volcanoes can — and do — influence the global climate over time periods of a few years but this is achieved through the injection of sulfate aerosols into the high reaches of the atmosphere during the very large volcanic eruptions that occur sporadically each century.

Unless we had magical insulation or back radiation, in the simple model no heat could pile up in the atmosphere during the night.

However, CO2 is also released back to the atmosphere during winter and autumn.

Scientists have learned that about 1,361 watts per square meter of solar energy reaches Earth's outermost atmosphere during the sun's quietest periods.

A recent report by Principia Scientific International's (PSI) Martin Mlynczak alongside NASA tracked infrared emissions from the Earth's upper atmosphere during and following a solar storm last March.

Based on the empirical evidence of the laboratory experiments, it is quite possible that the increasing CO2 in the atmosphere during interglacial periods could have amplified the warming already occurring.

This is equivalent to the atmosphere during the night.

In the case of natural gas, you have to take into account how much methane and CO2 are lost to the atmosphere during the mining, storage, and transport.

Because the sea surface gets colder, there is less evaporation, and thus less heat transfer from the ocean to the atmosphere during the time it takes for the water to reach the Arctic Ocean.

Most of the latent heat contained in water vapour is subsequently released to the atmosphere during the formation of precipitating clouds, although a minor amount may be returned directly to the surface during dew or frost deposition.

Thus, there is a strong potential that the added dust in the atmosphere during this drought could have intensified the drought by reducing precipitation over the plains.

Past studies have reported significant changes in the earth's atmosphere during the extended solar minimum, from 2007 to 2009 (Emmert et al. 2010; Ermolli et al. 2012).

«It is widely assumed that biomass combustion would be inherently «carbon neutral» because it only releases carbon taken from the atmosphere during plant growth.

During 1980s I listened to some academical lectures concerning the correlation between global temperature and CO2 content in atmosphere during glacials and interglacials.

Intriguingly, the rate of carbon release (in the form of methane) into the atmosphere during the PETM was similar to the rate at which we are pumping it out today as CO2.

Dinneen says that the ILUC emissions estimates in the look - up table were never adjusted to account for ARB's own assumption in the ISOR that not all the carbon in the cleared woody material is released to the atmosphere during the year following the clearing — i.e., since some of the wood is used for building material, it continues to sequester carbon after the clearing event.

If the slower cooling phase is still evident (as there is more CO2 in the atmosphere during the peak of the warm cycle which should keep temperatures warmer for longer) then this should constitute empirical evidence for CO2's effects on the climate.

1) On dry savannas in Africa the surface temperature of clear climate during daytime can reach about 50 C, but during nighttime can cool down until about zero C. However, CO2 content in atmosphere during all the time is the same, which proves that the carbon dioxide as greenhouse gas in atmosphere has no distinguishable influence on climate temperature.

Steven Davis of the University of California, Irvine and Robert Socolow of Princeton University in the US report in the journal Environmental Research Letters that existing power plants will emit 300 billion tonnes of additional carbon dioxide into the atmosphere during their lifetimes.

Mauritsen said the warming of the upper ocean and the atmosphere during the summer through reduced cooling around Europe results in the stronger transport of heat into the Arctic, which is actually «pristine» in general.

Kind of like spewing uncombusted hydrocarbons into the upper atmosphere during countless flights a day just doing business.

With the conventional chip bag, you're taking fossil based fuels out of the ground, and converting them into packaging with the associated generation of green house gas to the atmosphere during that production process.

Fig. 2 The CO2 concentration of the atmosphere during the Holocene, measured in the ice cores from Antarctica until 1958, afterwards Mauna Loa.