Sentences with phrase «warmer conditions increase»

In general warmer conditions increase biological activity.

For instance, warmer conditions increase droughts and reduce fuel quantity.

Not exact matches

It will be cheaper, they tell us, to adjust to increased storm damage, build more dikes and seawalls, relocate people and pay the costs of increased air - conditioning than it would be to take steps to slow global warming.

• We are increasing the amount of carbon dioxide in the air, causing changing climatic conditions and global warming.

And again: The IPCC claimed that there was an increase in extreme weather conditions as a result of human - induced global warming.

Basic care for all newborns should include promoting and supporting early and exclusive breastfeeding, keeping the baby warm, increasing hand washing and providing hygienic umbilical cord and skin care, identifying conditions requiring additional care and counselling on when to take a newborn to a health facility.

Warmer conditions reduce the solubility of oxygen from the atmosphere and increase oxygen consumption because the biological respiration processes are boosted.

The hourlong documentary examines how Arctic warming may be increasing storms» intensity and altering their paths, and how countries such as the Netherlands are creating climate - adaptive cities to respond to changing conditions

The strength and path of the North Atlantic jet stream and the Greenland blocking phenomena appear to be influenced by increasing temperatures in the Arctic which have averaged at least twice the global warming rate over the past two decades, suggesting that those marked changes may be a key factor affecting extreme weather conditions over the UK, although an Arctic connection may not occur each year.

Thanks to global warming, waterways that make up important habitat for fish are likely to experience an increased frequency of such extreme conditions.

Projected global warming will likely decrease the extent of temperate drylands by a third over the remainder of the 21st century coupled with an increase in dry deep soil conditions during agricultural growing season.

Warmer weather may increase the frequency of an unusual climatic condition called a rain - on - snow event, says earth system scientist Jaakko Putkonen of the University of Washington, Seattle.

European wheat production areas have to prepare for greater harvest losses in the future when global warming will lead to increased drought and heat waves in southern Europe, and wet and cool conditions in the north, especially at the time of sowing.

The coldest night of the winter in this region has warmed by about 7 degrees Fahrenheit in the past 50 years, creating favorable conditions for the southern pine beetle to increase its range.

The observed increase in freshwater content will affect the conditions in all Greenland fjords and may ultimately affect the global ocean currents that keep Europe warm.

By making conditions favorable for mosquitoes, «warmer temperatures increase transmission, so you're going to increase the number of people you treat,» she said.

Dr Li said the latest research findings give a better understanding of changes in human - perceived equivalent temperature, and indicate global warming has stronger long - term impacts on human beings under both extreme and non-extreme weather conditions, suggesting that climate change adaptation can not just focus on heat wave events, but should be extended to the whole range of effects of temperature increases.

«It confirms that the during the Medieval Warm Period between 1080 and 1430 the oscillation index was in an unusually prolonged positive phase, which brings increased rain to Scotland and drier conditions in the western Mediterranean,» says Baker, of the UNSW Connected Waters Initiative Research Centre.

Professor Grant Bigg, from the University's Department of Geography, said: «Many people may associate warmer seas with the pleasant weather conditions they're used to experiencing while on holiday, but the fact of the matter is that an increase in sea temperatures is having a huge impact on the world's weather.

The report lists 30 cities that face increased health risks from heat waves worsened by global warming, based on a combination of four factors: average number of summer days with «oppressive» summer heat, the percentage of households without central air conditioning, ground - level ozone levels, and the percentage of households below the poverty line.

«(VII) standards for practices and materials to achieve cool roofs in residential buildings, taking into consideration reduced air conditioning energy use as a function of cool roofs, the potential reduction in global warming from increased solar reflectance from buildings, and cool roofs criteria in State and local building codes and in national and local voluntary programs, without reduction of otherwise applicable ceiling insulation standards; and

Although warmer winters favor an increased mean population size, density - dependent feedback can cause the local population to be less buffered against occasional poor environmental conditions (cold winters).

Bacteria, however, have remained Earth's most successful form of life — found miles deep below as well as within and on surface rock, within and beneath the oceans and polar ice, floating in the air, and within as well as on Homo sapiens sapiens; and some Arctic thermophiles apparently even have life - cycle hibernation periods of up to a 100 million years while waiting for warmer conditions underneath increasing layers of sea sediments (Lewis Dartnell, New Scientist, September 20, 2010; and Hubert et al, 2010).

For example, Sturrock et al. (2011) estimate that a) Dothistroma needle blight (Dothistroma septosporum or D. pini), whose primary host in Montana is ponderosa pine, will have reduced or increased impacts, depending on warmer and drier or wetter conditions, respectively; and b) Armillaria root disease (Armillaria spp.), which generally affects Douglas - fir and grand fir, will have increased impacts under warmer, drier conditions, but no change under warmer, wetter conditions.

In Montana, increased fire frequency is associated with warmer spring temperatures and drier summer conditions (Heyerdahl et al. 2008; Morgan et al. 2008), often associated with El Niño.

Similarly, the combination of increased warming and drought conditions is the likely cause of recent rapid increases in background (non-catastrophic) forest mortality rates in Montana and the interior West (van Mantgem et al. 2009).

Warmer, drier climate phases can particularly increase fire risk when they follow cooler, wetter conditions that increase fire fuel availability via increased vegetation growth and reduced fire activity (Heyerdahl et al. 2008).

UHI effects have been documented in city environments worldwide and show that as cities become increasingly urbanised, increasing energy use, reductions in surface water (and evaporation) and increased concrete etc. tend to lead to warmer conditions than in nearby more rural areas.

Direct effects of climate change on trees and forests, such as warmer, wetter conditions improving forest productivity or warmer, drier conditions increasing tree mortality, will be secondary to the impacts of altered forest disturbance regimes, such as changes in forest fire behavior and area burned.

Warmer conditions would also have encouraged faster movement and increased bedrock erosion.

The phase of the Pacific Decadal Oscillation that leads to warmer conditions may also prolong and intensify the fire season (Heyerdahl et al. 2008; Jolly et al. 2015; Abatzoglou and Williams 2016), and it is clear that years with protracted or widespread wildland fire or increased fire severity are correlated with drought (Littell et al. 2009; van Mantgem et al. 2013).

Ground - level ozone formation increases under the hot and stagnant conditions that are expected to increase in a warmer world.

This chemical weathering process is too slow to damp out shorter - term fluctuations, and there are some complexities — glaciation can enhance the mechanical erosion that provides surface area for chemical weathering (some of which may be realized after a time delay — ie when the subsequent warming occurs — dramatically snow in a Snowball Earth scenario, where the frigid conditions essentially shut down all chemical weathering, allowing CO2 to build up to the point where it thaws the equatorial region, at which point runaway albedo feedback drives the Earth into a carbonic acid sauna, which ends via rapid carbonate rock formation), while lower sea level may increase the oxidation of organic C in sediments but also provide more land surface for erosion... etc..

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Massage for hair loss performed by a trained massage therapist will increase blood flow to the hair follicles, condition the scalp and enhance the strength of the roots. Kneading during a massage warms the skin and opens up the blood vessels.

8A / 12A switchable Level 1 charging cable CHAdeMO DC quick charge port Battery warming system MiEV remote system (pre-activated air conditioning, heater and timer battery charging) Approaching Vehicle Audio System (AVAS) for alerting pedestrians Charging Times: 3 22 hours for 8amp 14 hours for 12 amp 7 hours with 240V / 15A Level 2 charging system Less than 30 minutes to 80 % full with CHAdeMO Level 3 DC Quick Charger Driving Modes: «D» — allows maximum performance as it generates 100 % torque in direct response to accelerator input «ECO» — helps maximize energy usage («fuel economy») by slightly reducing overall power output to reduce the rate of battery consumption «B» — increases regenerative brake biasing to augment energy recycling (with 100 % of power production available)

The system activates to warm the occupants more quickly; this reduces the load on the air conditioning system which further increases the fuel efficiency.

They are competition - oriented tires, optimized for warm, dry conditions to increase cornering and handling capability.

Over the years, mild weather conditions in the fall and early spring warming have contributed to a steady increase in ticks and cases of tick - borne diseases, especially in the Northeast.

With everyone agreed that the day's conditions had been perfect for beginners just getting used to riding their first waves, attentions were soon transfixed on the horizon as the sun sank below the clouds, lighting up the ocean and gradually increasing its descent into the waves until all that remained was a warm glow on the horizon.

The reason you see such a sharp upward slope in the dotted red line between AD 500 and 1000 is that the relatively warm conditions indicated by the temperature reconstruction is suggesting a fast rate of SLR increase.

Therefore, if conditions allow the glacier surface to warm to 0 C, the amount of ablation that can be sustained by a given energy input increases dramatically.

A subset of Earth System Models (ESMs) project that El Niño - like conditions will progressively increase in coming decades as sea - surface temperatures in the tropical Pacific warm, implying increased drought and forest dieback in the Amazon.

Soundbite version: «Global warming is expected to increase sea surface temperatures, create a thicker and warmer ocean surface layer, and increase the moisture in the atmosphere over the oceans — all conditions that should lead to a general increase in hurricane intensity and maybe frequency.»

Recent work suggests an increase in recent decades in the occurrence of QRA - favorable conditions and associated extreme weather, possibly linked to amplified Arctic warming and thus a climate change influence.

«The climate patterns responsible for the expected above - normal 2007 hurricane season continue to be the ongoing multi-decadal signal (the set of oceanic and atmospheric conditions that have spawned increased Atlantic hurricane activity since 1995), warmer - than - normal sea surface temperatures in key areas of the Atlantic Ocean and Caribbean Sea, and the El Nino / La Nina cycle»

At a certain point, nature will generate conditions to increase the warming.

Warmer, drier conditions can result in a stressed environment for trees — making them more susceptible to insect attack — and higher temperatures can increase the speed of insect development.

The surface heat capacity C (j = 0) was set to the equivalent of a global layer of water 50 m deep (which would be a layer ~ 70 m thick over the oceans) plus 70 % of the atmosphere, the latent heat of vaporization corresponding to a 20 % increase in water vapor per 3 K warming (linearized for current conditions), and a little land surface; expressed as W * yr per m ^ 2 * K (a convenient unit), I got about 7.093.

(1) increased demand for heating fuels and electricity due to cooler winter and warmer summer conditions in 2007 than in 2006; (2) increased consumption of fossil fuels to generate electricity; and (3) a significant decrease (14.2 percent) in hydropower generation used to meet this demand.