Sentences with phrase «increase in warmer times»

The research also shows that the swings in Pacific temperatures tend to increase in warmer times — like now — but weakened by as much as 50 percent during the protracted cold of the last ice age.

Not exact matches

There is no evidence for significant increase of CO2 in the medieval warm period, nor for a significant decrease at the time of the subsequent little ice age.

Increase in bonding time Reduces postpartum depression Helps to lessen the amount of crying a baby does Helps the baby sleep better Reduces the stress level of the mother Betters the breastfeeding relationship Keeps blood sugar regulated Keeps baby's body warmer

In fact, it was recently reported that their network is «warming» to Trump, at the same time that his actions are an increasing cause of alarm for anyone worried about our country's institutions.

There are three main time scales to consider when it comes to warming: annual temperature variation from factors like warming in the Pacific Ocean during El Niño years, decadal temperature swings and long - term temperature increases from global warming.

One factor is that researchers have found warmer temperatures increase the number of young produced by the gloomy scale insect — a significant tree pest — by 300 percent, which in turn leads to 200 times more adult gloomy scales on urban trees.

The «residence time» of the very warm water in the Torres Strait and the Northern Great Barrier Reef was exceptionally long, which increased the thermal stress on the coral.

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.

As a result of atmospheric patterns that both warmed the air and reduced cloud cover as well as increased residual heat in newly exposed ocean waters, such melting helped open the fabled Northwest Passage for the first time [see photo] this summer and presaged tough times for polar bears and other Arctic animals that rely on sea ice to survive, according to the U.S. Geological Survey.

Fact # 1: Carbon Dioxide is a Heat - Trapping Gas Fact # 2: We Are Adding More Carbon Dioxide to the Atmosphere All the Time Fact # 3: Temperatures are Rising Fact # 4: Sea Level is Rising Fact # 5: Climate Change Can be Natural, but What's Happening Now Can't be Explained by Natural Forces Fact # 6: The Terms «Global Warming» and «Climate Change» Are Almost Interchangeable Fact # 7: We Can Already See The Effects of Climate Change Fact # 8: Large Regions of The World Are Seeing a Significant Increase In Extreme Weather Events, Including Torrential Rainstorms, Heat Waves And Droughts Fact # 9: Frost and Snowstorms Will Still Happen in a Warmer World Fact # 10: Global Warming is a Long - Term Trend; It Doesn't Mean Next Year Will Always Be Warmer Than This YeIn Extreme Weather Events, Including Torrential Rainstorms, Heat Waves And Droughts Fact # 9: Frost and Snowstorms Will Still Happen in a Warmer World Fact # 10: Global Warming is a Long - Term Trend; It Doesn't Mean Next Year Will Always Be Warmer Than This Yein a Warmer World Fact # 10: Global Warming is a Long - Term Trend; It Doesn't Mean Next Year Will Always Be Warmer Than This Year

Climate change, resulting in more frost - free days and warmer seasonal air temperatures, can contribute to shifts in flowering time and pollen initiation from allergenic plant species, and increased CO2 by itself can elevate production of plant - based allergens.137, 15,16,17,18,19,138 Higher pollen concentrations and longer pollen seasons can increase allergic sensitizations and asthma episodes, 20,21,155,22 and diminish productive work and school days.138, 22,23

For the first time, scientists have shown a direct link between rising levels of carbon dioxide — or CO2 — in Earth's atmosphere and an increase in how much solar energy warms the ground.

-- 7) Forest models for Montana that account for changes in both climate and resulting vegetation distribution and patterns; 8) Models that account for interactions and feedbacks in climate - related impacts to forests (e.g., changes in mortality from both direct increases in warming and increased fire risk as a result of warming); 9) Systems thinking and modeling regarding climate effects on understory vegetation and interactions with forest trees; 10) Discussion of climate effects on urban forests and impacts to cityscapes and livability; 11) Monitoring and time - series data to inform adaptive management efforts (i.e., to determine outcome of a management action and, based on that outcome, chart future course of action); 12) Detailed decision support systems to provide guidance for managing for adaptation.

We assess the heat content change from both of the long time series (0 to 700 m layer and the 1961 to 2003 period) to be 8.11 ± 0.74 × 1022 J, corresponding to an average warming of 0.1 °C or 0.14 ± 0.04 W m — 2, and conclude that the available heat content estimates from 1961 to 2003 show a significant increasing trend in ocean heat content.

For example, one model reaches 38 percent of the maximum warming in the first decade after a step increase in CO2 concentration, while another model reaches 61 percent of the maximum warming in this time period.

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..

The average flood height increased by about 4 feet in New York between the two time periods and with continued warming, larger and more extreme storms along with even higher sea level is likely to cause more frequent and intense flooding.

«We show that at the present - day warming of 0.85 °C about 18 % of the moderate daily precipitation extremes over land are attributable to the observed temperature increase since pre-industrial times, which in turn primarily results from human influence,» the research team said.

However, in comparison with the solar case, the FIR photosphere of alpha Cen A appears marginally cooler, Tmin = T160mu = 3920 + / -375 K. Beyond the minimum near 160mu, the brightness temperatures increase and this radiation likely originates in warmer regions of the chromosphere of alpha Cen A. To the best of our knowledge this is the first time a temperature minimum has been directly measured on a main - sequence star other than the Sun.

«Warm compresses increase blood flow and loosen the oil to help unclog the glands,» says Payal Patel, MD, a clinical instructor in the department of ophthalmology at NYU Langone Medical Center, who recommends applying a warm washcloth to the eyelid for one to two minutes three or four times a Warm compresses increase blood flow and loosen the oil to help unclog the glands,» says Payal Patel, MD, a clinical instructor in the department of ophthalmology at NYU Langone Medical Center, who recommends applying a warm washcloth to the eyelid for one to two minutes three or four times a warm washcloth to the eyelid for one to two minutes three or four times a day.

In addition to a good warm - up, Altman suggests only a 10 - 15 % increase in mileage, or time, each week to prevent injurIn addition to a good warm - up, Altman suggests only a 10 - 15 % increase in mileage, or time, each week to prevent injurin mileage, or time, each week to prevent injury.

In Ancient Greece, Hippocrates advised that lentils were the food to promote potency.1 In the Late Middle Ages, scholars believed that warm, moist foods like egg yolks could enhance amorous feelings (while cold foods like cucumber would `' extinguish lust»).2 And, to increase his virility, legendary lover Casanova is said to have routinely breakfasted on as many as 50 oysters at a time.3

If a larger mass of warm air has to pass through it, more energy is transferred, through the evaporator's fins (so that even the evaporator's design and, in particular, its exchange surface play an important part) from the air to the liquid refrigerant allowed inside it by the TEV or orifice tube so it expands more and, along with the absolute pressure inside the evaporator, the refrigerant's vapor superheat (the delta between the boiling point of the fluid at a certain absolute pressure and the temperature of the vapour) increases, since after expanding into saturated vapour, it has enough time to catch enough heat to warm up further by vaporizing the remaining liquid (an important property of a superheated vapour is that no fluid in the liquid state is carried around by the vapour, unlike with saturated vapour).

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)

Those suits keep your body warm and increase your buoyancy, so you will be able to spend more time in the ocean.

As spring rushes into summer in Utah, the time spent out of doors each day has increased exponentially: we want to be surrounded by bright light, warm air, and beautiful landscapes.

GHG continue to increase in amounts in the atmosphere and as such, over time more warming inevitably continues though there may be breaks for short periods, and some cooling, as already discussed at great length regarding aerosols.

If potentially pernicious effects such as global warming are human - driven, then it is reasonable and sensible to ask what is fueling the recent skyrocketing increase of absolute global human population numbers that, in turn, are destabilizing Earth's global ecosystems and dissipating Earth's limited resources in our time.

This week, PNAS published our paper Increase of Extreme Events in a Warming World, which analyses how many new record events you expect to see in a time series with a trend.

«The major trends over time are a wintertime WVP and LWP increase south and southwest of Greenland also seen in precipitation, consistent with modification of continental air flowing out over increasingly warmer waters.

In context of current increased forcing and in consideration of all relevant natural and forced events and time scale, it is valid to say that this is expected in a warming worlIn context of current increased forcing and in consideration of all relevant natural and forced events and time scale, it is valid to say that this is expected in a warming worlin consideration of all relevant natural and forced events and time scale, it is valid to say that this is expected in a warming worlin a warming world.

«This uncertainty is illustrated by Pollard et al. (2015), who found that addition of hydro - fracturing and cliff failure into their ice sheet model increased simulated sea level rise from 2 m to 17 m, in response to only 2 °C ocean warming and accelerated the time for substantial change from several centuries to several decades.»

In other words, the same natural forcings that appear responsible for the modest large - scale cooling of the LIA should have lead to a cooling trend during the 20th century (some warming during the early 20th century arises from a modest apparent increase in solar irradiance at that time, but the increase in explosive volcanism during the late 20th century leads to a net negative 20th century trend in natural radiative forcingIn other words, the same natural forcings that appear responsible for the modest large - scale cooling of the LIA should have lead to a cooling trend during the 20th century (some warming during the early 20th century arises from a modest apparent increase in solar irradiance at that time, but the increase in explosive volcanism during the late 20th century leads to a net negative 20th century trend in natural radiative forcingin solar irradiance at that time, but the increase in explosive volcanism during the late 20th century leads to a net negative 20th century trend in natural radiative forcingin explosive volcanism during the late 20th century leads to a net negative 20th century trend in natural radiative forcingin natural radiative forcing).

Because that's about how much time we have to stop the increase in greenhouse gas emissions and begin steep reductions that will bring emissions to near zero within another ten years at most, if we are to have any hope of avoiding the most catastrophic consequences of global warming.

The paper appears to conclude that if we wait 20 years to begin reducing GHG emissions, assuming a modest amount of mitigation in the short term, we will have to reduce emissions at a 3 to 7 times greater rate than if we start now in order to keep warming to a 3 degree C increase around 2100.

This is the 2nd time in recent weeks that someone has claimed that there's a widespread assertion that the warming should be accelerating due to CO2 increases

However, it is important to keep in mind that we might easily more than double it if we really don't make much effort to cut back (I think the current estimated reserves of fossil fuels would increase CO2 by a factor of like 5 or 10, which would mean a warming of roughly 2 - 3 times the climate sensitivity for doubling CO2 [because of the logarithmic dependence of the resulting warming to CO2 levels]-RRB-... and CO2 levels may be able to fall short of doubling if we really make a very strong effort to reduce emissions.

Terrell Johnson, reporting on a recent NASA publication concluding that deep ocean temperatures have not increased since 2005 (http://www.weather.com/science/environment/news/deep-ocean-hasnt-warmed-nasa-20141007): «While the report's authors say the findings do not question the overall science of climate change, it is the latest in a series of findings that show global warming to have slowed considerably during the 21st century, despite continued rapid growth in human - produced greenhouse gas emissions during the same time.»

«In a scenario of zeroed CO2 and sulfate aerosol emissions, whether the warming induced by specified constant concentrations of non-CO2 greenhouse gases could slow the CO2 decline following zero emissions or even reverse this trend and cause CO2 to increase over time is assessed.

I've been to the Arctic three times for the newspaper since 2003 — visiting the North Slope, North Pole, and Greenland to examine what mix of human and natural forces is driving the warming and ice retreats and the implications of having increasing amounts of open water in summers in a region increasingly seen as a resource trove and shortcut for shipping.

In my opinion, this is a question of the time scale considered: the variations from year to year are obviously dominated by weather, and also decadal variations — such as the warming (probably the increase of the flow) from 1990 to the middle of the 2000s and the subsequent cooling (slowdown of the flow)-- are likely to be mainly natural variations.

What most people seem to forget here, is that on one hand there are fundamental thermodynamical arguments which demand that hurricane intensity increase over time, while on the other hand, there are these two big chunks of ice sitting in both polar regions, which will counteract the warming process in their own special way.

What this regional cooling data in more current times indicates to me is that it must be getting really hot in other places (& not all places are warming in lock - step), or we wouldn't be having this increase in the AVERAGE of global temps.

We reg folks only have time for news headlines (not sci articles), so the man - in - the - street reads, «Katrina not caused by GW,» & thinks «GW has been disproved & I can rest easy,» while his wife reads in the Drs office, «GW increasing Hurricane intensity» (a reporter read «warming oceans increasing hurricane intensity» and got confused, and I don't fault him for it, bec he / she's very much like that person - in - the - street).

With warmer SSTs, I would imagine there will be more storms like Wilma that will increase their intensity from TS to cat 4/5 level in a very short period of time.

Even in a time of global warming, an increase in ice sheet melting or deep water upwelling can cool the atmosphere relative to the long term trend.

However, at the same time, there's been the steady increase in subtropical ocean surface temperatures in the Atlantic Warm Pool, leading to record water temperatures off the US east coast in winter, which tends to fuel more extreme storms (via the increase in water vapor pressure over the warmer ocean).

Or, trying to «correct» for the different lifetimes of the gases using Global Warming Potentials, over a 100 - year time horizon (which still way under - represents the lifetime of the CO2), you get that the methane would be equivalent to increasing CO2 to about 500 ppm, lower than 750 because the CO2 forcing lasts longer than the methane, which the GWP calculation tries in its own myopic way to account for.

Water from the melting ice makes the oceans rise, only a fraction of an inch a year but, in the fullness of time, enough to let the currents increase their flow over the northern sill, bringing ever more warm water into the gelid Arctic.

In terms of the aerosols: If you want to argue really simplistic, you could still explain what is seen in Dave's NH - SH time series: due to the larger thermal inertia of the SH, you would expect slower warming there with greenhouse gas forcing, so an increase in NH - SH early on, which would then be reduced as aerosol forcing becomes stronger in the NIn terms of the aerosols: If you want to argue really simplistic, you could still explain what is seen in Dave's NH - SH time series: due to the larger thermal inertia of the SH, you would expect slower warming there with greenhouse gas forcing, so an increase in NH - SH early on, which would then be reduced as aerosol forcing becomes stronger in the Nin Dave's NH - SH time series: due to the larger thermal inertia of the SH, you would expect slower warming there with greenhouse gas forcing, so an increase in NH - SH early on, which would then be reduced as aerosol forcing becomes stronger in the Nin NH - SH early on, which would then be reduced as aerosol forcing becomes stronger in the Nin the NH.