Sentences with phrase «causes more warm water»

Not exact matches

It does indeed cause some warming of our planet, and we should thank Providence for that, because without the greenhouse warming of CO2 and its more potent partners, water vapor and clouds, the earth would be too cold to sustain its current abundance of life.

Before you touch your face, make sure to wash your hands with soap and warm water to clean your hands of bacteria that can cause more blemishes.

Many lakes have been warming with a changing climate, and clearer water caused by invasive zebra mussels provides more sunlight for algae to grow in thicker mats.

A rather straightforward calculation showed that doubling the level of carbon dioxide in the atmosphere... which would arrive in the late 21st century if no steps were taken to curb emissions... should raise the temperature of the surface roughly one degree C. However, a warmer atmosphere would hold more water vapor, which ought to cause another degree or so of warming.

Warmer air temperatures cause more water containing the heavier isotopes oxygen - 18 or deuterium to evaporate from the surrounding ocean.

Moreover, the warming makes the atmosphere damper (providing still more water vapor) and may cause the stratosphere to heat up, speeding the chemical reactions that destroy ozone.

A possible cause for the accelerated Arctic warming is the melting of the region's sea ice, which reduces the icy, bright area that can reflect sunlight back out into space, resulting in more solar radiation being absorbed by the dark Arctic waters.

Totten Glacier, the largest glacier in East Antarctica, is being melted from below by warm water that reaches the ice when winds over the ocean are strong — a cause for concern because the glacier holds more than 11 feet of sea level rise and acts as a plug that helps lock in the ice of the East Antarctic Ice Sheet.

Indeed, conventional wisdom held that higher levels of aerosol pollution in the atmosphere should cool the earth's climate because aerosols can increase cloudiness; they not only reduce precipitation, which raises the water content in clouds, but they also increase the size of the individual water droplets, which in turn causes more warming sunlight to be reflected back into space.

Another hypothesis is that rapidly warming water in the Gulf of Maine, which includes Cape Cod Bay and waters north to Nova Scotia, could be luring turtles farther north than they once ventured, causing more to become trapped on their southbound journey when the water cools in the fall.

The knock - on effects of such a transition would be huge — they would cause marked increase of warming at the pole, since open water absorbs more of the sun's energy than ice - covered seas.

If they begin to melt, however — particularly as they're exposed to warmer ocean water — the shelves become thinner and the grounding line begins to retreat backward, causing the glacier to become less stable and making the ice shelf more likely to break.

The clearest impact of warming on drought is when higher temperatures cause more evaporation and increase water demand, as has happened with this drought.

A warming atmosphere causes more evaporation, meaning more water is available for precipitation.

Warmer air also causes more water to evaporate from the soil.

Remember that direct greenhouse effect from CO2 is quite small; the predictions rely on positive feedback from other effects (particularly water vapour feedbacks, a far more significant greenhouse gas) to cause substantial warming.

However, the surface warming caused by human - produced increases in carbon dioxide, methane, and other greenhouse gases leads to a large increase in water vapor, since a warmer atmosphere holds more moisture.

And that additional water vapour would in turn cause further warming - this being a positive feedback, in which carbon dioxide acts as a direct regulator of temperature, and is then joined in that role by more water vapour as temperatures increase.

Scientists working with the World Weather Attribution team revealed that climate change made the warm waters that caused the bleaching last year up to 175 times more likely.

leave cap off make sure fill with antifreeze and start car allow it to warm up and watch u should be able to see the water flow this will allow the air to come out per air pockets are a big cause... now buy a new radiator cap per this also small but cause a big prob... also while watching the water flow flow if bubbles stay present it could be head gasket this pushes combustion gas thru and can cause antifreeze to dicipate hence why u keep having to put more unless yur pump leaking or hose this the only other way u will get low on anti freeze... hope this helps it took me a while to figure out so i did nt have to spend lots of cash on a mech that wouldnt probably now this either top secrets lol... they wont tell u its all biz... hope this helps

«Note: LOTI provides a more realistic representation of the global mean trends than dTs below; it slightly underestimates warming or cooling trends, since the much larger heat capacity of water compared to air causes a slower and diminished reaction to changes.»

But since it is linear, if the temperature rises then the water vapour will run away, because the higher temperature leads to more water vapour which causes more greenhouse warming which leads to higher temperatures.

As the atmosphere warms it can hold more water; that additional water vapor provides more of the warming than is directl caused by CO2.

--- ignorance about atmospheric chemistry really shows here...... snip --- «Moreover, the CO2 that is supposedly causing «catastrophic» warming represents only 0.00035 of all the gases in the atmosphere (1.25 inches out of a 100 - yard football field), and proposals to control this vital plant nutrient ignore a far more critical greenhouse gas: water vapor.»

Simple physics dictates that with less sea ice there is magnified warming of the Arctic due to powerful albedo feedback; this in turn reduces the equator to pole temperature gradient which slows the jet stream winds causing them to become more meridional; this combined with 4 % more water vapor in the atmosphere (compared to 3 decades ago) is leading to much more extremes in weather.

Warmer temperatures causes more water vapor, which causes more warmth, etc..

Warming must occur below the tropopause to increase the net LW flux out of the tropopause to balance the tropopause - level forcing; there is some feedback at that point as the stratosphere is «forced» by the fraction of that increase which it absorbs, and a fraction of that is transfered back to the tropopause level — for an optically thick stratosphere that could be significant, but I think it may be minor for the Earth as it is (while CO2 optical thickness of the stratosphere alone is large near the center of the band, most of the wavelengths in which the stratosphere is not transparent have a more moderate optical thickness on the order of 1 (mainly from stratospheric water vapor; stratospheric ozone makes a contribution over a narrow wavelength band, reaching somewhat larger optical thickness than stratospheric water vapor)(in the limit of an optically thin stratosphere at most wavelengths where the stratosphere is not transparent, changes in the net flux out of the stratosphere caused by stratospheric warming or cooling will tend to be evenly split between upward at TOA and downward at the tropopause; with greater optically thickness over a larger fraction of optically - significant wavelengths, the distribution of warming or cooling within the stratosphere will affect how such a change is distributed, and it would even be possible for stratospheric adjustment to have opposite effects on the downward flux at the tropopause and the upward flux aWarming must occur below the tropopause to increase the net LW flux out of the tropopause to balance the tropopause - level forcing; there is some feedback at that point as the stratosphere is «forced» by the fraction of that increase which it absorbs, and a fraction of that is transfered back to the tropopause level — for an optically thick stratosphere that could be significant, but I think it may be minor for the Earth as it is (while CO2 optical thickness of the stratosphere alone is large near the center of the band, most of the wavelengths in which the stratosphere is not transparent have a more moderate optical thickness on the order of 1 (mainly from stratospheric water vapor; stratospheric ozone makes a contribution over a narrow wavelength band, reaching somewhat larger optical thickness than stratospheric water vapor)(in the limit of an optically thin stratosphere at most wavelengths where the stratosphere is not transparent, changes in the net flux out of the stratosphere caused by stratospheric warming or cooling will tend to be evenly split between upward at TOA and downward at the tropopause; with greater optically thickness over a larger fraction of optically - significant wavelengths, the distribution of warming or cooling within the stratosphere will affect how such a change is distributed, and it would even be possible for stratospheric adjustment to have opposite effects on the downward flux at the tropopause and the upward flux awarming or cooling will tend to be evenly split between upward at TOA and downward at the tropopause; with greater optically thickness over a larger fraction of optically - significant wavelengths, the distribution of warming or cooling within the stratosphere will affect how such a change is distributed, and it would even be possible for stratospheric adjustment to have opposite effects on the downward flux at the tropopause and the upward flux awarming or cooling within the stratosphere will affect how such a change is distributed, and it would even be possible for stratospheric adjustment to have opposite effects on the downward flux at the tropopause and the upward flux at TOA).

However, higher temperatures do cause an increased chance of heavy precipitation events, and it is likely that the flooding in some of this year's U.S. flooding disasters were significantly enhanced by the presence of more water vapor in the air due to global warming.

At the meeting this week, scientists are reporting more on the extent of Arctic warming — the waters, particularly near Alaska and Russia, were up to 9 degrees Fahrenheit above average — and narrowing down the causes.

Increased melting in the warmer summer is causing the internal drainage system of the ice sheet to accommodate more melt - water, without speeding up the flow of ice toward the oceans, the journal Nature reports.

Totten Glacier, the largest glacier in East Antarctica, is being melted from below by warm water that reaches the ice when winds over the ocean are strong — a cause for concern because the glacier holds more than 11 feet of sea level rise and acts as a plug that helps lock in the ice of the East Antarctic Ice Sheet.

Their causes range from completely unpredictable events like volcanic eruptions (which have mainly local effects) to more regular phenomena such as «El Niño» (a warming of the surface waters of the tropical Pacific that occurs every three to five years, temporarily affecting weather world - wide).

Also part of the explanation is the claim that more humid air results in more precipitation, but again I'm unclear on why warmer air can cause more water to be evaporated, but warmer air does not by the same mechanism prevent the same water from condensing.

Warmer water from the engine block causes metal in the thermostat to expand which widens the opening allowing more water to move from block to radiator for disposal.

Lake - effect snow happens when moisture from warmer lake waters mixes with cold air coming from the north, causing more than 2 to 3 inches of snow an hour.

The paper discusses that melting ice will decrease the salinity of the ocean waters around Antarctica, which will cause decreased mixing with the relatively warmer deep ocean waters, reducing sea surface temperatures, causing more sea ice to form.

The Charney Report stated that numerical modelers of global climate had estimated that the modest warming caused by carbon dioxide would be greatly amplified by a more powerful warming from an increase in water vapor, particularly in the tropics.

Such events are consistent with the effects of global warming, which is expected to cause more heavy precipitation because of a greater amount of water vapor in the atmosphere.»

We do not need models to anticipate that significant rises in atmospheric CO2 concentrations harbor the potential to raise temperatures significantly (Fourier, 1824, Arrhenius, 1896), nor that the warming will cause more water to evaporate (confirmed by satellite data), nor that the additional water will further warm the climate, nor that this effect will be partially offset by latent heat release in the troposphere (the «lapse - rate feedback»), nor that greenhouse gas increases will warm the troposphere but cool the stratosphere, while increases in solar intensity will warm both — one can go on and on

The theory of AGW says that extra CO2 causes a minor warming (less than 0.5 degree) which then causes the atmosphere to absorb more water vapour.

When fall arrives and cold air moves in again, all the energy stored in the water gets released into the atmosphere, which, in turn, causes the air above the water to warm up more than usual.

This snowpack accumulation near the poles, which gets its water via the Arctic and Antarctic oceans, that in turn rob it from equatorial latitudes of our oceans, also results in a reduction in the earth's spin axis moment of inertia and causes the spin rate to increase as evidenced in the recent history of the rate at which Leap Seconds are added to our calendar (see Wysmuller's Toucan Equation for more on this evidence that during this warm time with much greater polar humidity, earlier seasonal, later seasonal and heavier snows are beginning to move water vapor from the oceans to the poles to re-build the polar ice caps and lead us into a global cooling, while man - made CO2 continues to increase http://www.colderside.com/faq.htm).

A temperature rise (from whatever cause) would evaporate more water from the sea into the atmosphere, this would cause more warming and set up a feedback of ever escalating temperatures and water vapour levels.

Totten Glacier, the largest glacier in East Antarctica, is being melted from below by warm water that reaches the ice when winds over the ocean are strong — a cause for concern because the glacier holds more than 11 feet of sea level rise and acts as a plug that helps lock in the ice...

Even though La Niña produces an overall cooling effect over the eastern Pacific, the associated strengthening of the subtropical high - pressure system and trade winds causes warm water to accumulate more in the western Pacific.

However, the surface warming caused by human - produced increases in carbon dioxide, methane, and other greenhouse gases leads to a large increase in water vapor, since a warmer atmosphere holds more moisture.

Note 1: A simple hotspot explanation summarized from this article: Increasing CO2 levels causes atmosphere to warm; then atmosphere causes Earth's surface to warm; warming of oceans cause evaporation; increased evaporation leads to more water vapor in the upper troposphere; water vapor is a powerful greenhouse gas that warms the atmosphere even more (positive water vapor feedback); the Earth's surface warms even more; and then auto «repeat and rinse» until Earth's oceans boil, per an «expert.»

The theory is that increasing CO2 will cause a small bit of warming and this will increase evaporation rates (which occur fastest in the tropics) and dumps more water vapour in the atmosphere (water vapour is by far a more potent greenhouse gas than CO2) and this feedback amplification is meant to continue until Earth settles down and finds a new equilibrium temperature.

(right) With the transition from dimming to brightening (1980s — 2000s), the enhanced greenhouse effect has no longer been masked, causing more rapid warming, stronger evaporation / LH, and an intensification of the water cycle.

These effects are relatively well understood in the lowest level of the atmosphere, the troposphere, where increased warming leads to greater evaporation, causing more water vapour and so further warming, although this is offset to some extent through the formation of clouds that reflect incoming sunlight back into space.