Sentences with phrase «less water evaporation»

But should one not expect less water evaporation with decreased insolation?

Not exact matches

The main advantages of drip irrigation are that it conserves water because less is lost to evaporation, and it efficiently delivers water to individual plants.

Less than one percent of the world's water is liquid fresh water, and scientific studies suggest that a majority of U.S. and global fresh water is now at risk because of increasing consumption, evaporation and pollution.

In addition, less ice cover can lead to more evaporation and lower water levels while warmer water contributes to more algal blooms and impaired water quality, she says.

In addition, if there is less water being absorbed in the evaporation process, the sun's energy will just be going into the atmosphere, instead of being absorbed, and that could exacerbate global warming.

Less glacial runoff = less water to dam More drought = less water to dam Hotter, dryer conditions = faster evaporation from dam reservoLess glacial runoff = less water to dam More drought = less water to dam Hotter, dryer conditions = faster evaporation from dam reservoless water to dam More drought = less water to dam Hotter, dryer conditions = faster evaporation from dam reservoless water to dam Hotter, dryer conditions = faster evaporation from dam reservoirs.

... the higher up you go the less water vapor you normally get because it is too cold to have available water vapor (the rate of condensation strongly exceeds the rate of evaporation)... unless you warm it and «suddenly water vapor just appears» where it was mostly absent before.

However, with me at least, a bit part of the deal is the increased acidity reducing fish harvests, water shortages, droughts severely reducing crops (sure — more rain, but more over the ocean, less on land — and with greater evaporation before the water trickles to a dry stream bed), increased heat reducing rice production and other heat sensative crops, the heat waves, etc..

Evaporation from the soil means that plants will have less water.

For example, even though the volcanic effect is short - lived it will still have an impact on the water cycle - less evaporation because it's cooler therefore less water vapour, lowering temperature a bit more.

Part way there, but no quantitation yet: of the 3.77 W / m ^ 2 radiated back dowwnard, most goes to increased rate of evaporation of the water at the surface, and much less goes to increased mean temp increase at the surface; hence increased rate of non-radiative transfer of heat from surface to upper atmosphere, slight increase in rainfall as hydrological cycle is faster, and slight increase in cloud cover.

Slopes by angle can expose more or less volume of water to evaporation or flooding depending on degree of the slope to the height of water being displaced.

The lack of» water vapor» is, because: it was more water in Arctic ocean without ice cover as» insulation» - > water absorbed extra coldness and the currents brought extra coldness in North Atlantic = above the ocean is colder = less evaporation - > less water vapor produced - > less moisture going west from central Atlantic.

As for rainfall, in the simplest models, lowered temperatures decrease evaporation of water from the surface into the air; and less water vapor translates to less rain.

Again for example, during multidecadal periods when El Niño events dominate, the tropical North Atlantic trade winds would be on average weaker than «normal», there would be less evaporation, less cool subsurface waters would be drawn to the surface, and tropical North Atlantic sea surface temperatures would rise.

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.

LIA wasn't GLOBAL cooling; but colder in Europe, north America — because Arctic ocean had less ice cover - > was releasing more heat / was accumulating - > radiating + spreading more coldness — currents were taking that extra coldness to Mexican gulf — then to the Mediterranean — because Sahara was increasing creation of dry heat and evaporating extra water in the Mediterranean — to top up the deficit — gulf stream was faster / that was melting more ice on arctic also as chain reaction — Because Mediterranean doesn't have enough tributaries, to compensate for the evaporation deficit.

First, higher CO2 concentrations can lead to reduced evaporation, as the stomata, through which evaporation from plants takes place, conduct less water.

As the temperature increases, the water vapor pressure (hence by inference the water evaporation rate on non-dry surface) increases supralinearly; that is, a 1K increase from 288 K is much less than a 1K increase from 308K.

Decreased snowpack has brought less water into reservoirs (such as Lake Oroville, pictured, in Northern California), while increased temperatures have led to greater evaporation of surface water.

11 increased evaporation leaves salt behind, which increases the density dense water sinks and is replaced with less dense water Example: Mediterranean

to be used for drinking water Less evaporation from the storage reservoir Little loss of land No damage due to dam failure Pollutants such as mosquitoes and snails can not exist in the reservoirs Siltation does not create any problems Less vulnerable / below the ground surface in a shallow soil toward the impervious crystalline sub soil.

This causes more wave action which mixes colder water in from deep sea, this will cause less evaporation) 4) Negatively: more % water vapor in the atmosphere 5) Positively: evaporation itself causes more evaporation (difference in pressure causes wind and wind and heat together causes more evaporation)

If the surface is a water bed (seal to prevent evaporation) the range and rate of change would be less than if the surface was a foam mat.

Marine air temperatures and lower troposphere temperatures cool in response because the tropical Pacific is releasing less heat than normal through evaporation as a result of the cooler surface waters.

Early morning also tends to be when wind speeds are lower and, therefore, when water evaporation is less likely to occur.