Sentences with phrase «differences in temperature from»

In the past, a high difference in temperature from north to south helped drive a prevailing wind pattern called the Jet Stream which kept weather systems moving across the Northern Hemisphere.

As a Broadcast Meteorologist, we often (almost always) dictate a difference in temperature from the cities to the surrounding towns (colder at night in the towns, but warmer or colder during the afternoon depending).

The way I understand Gavin's explanation is the difference in temperatures from one day to the next for nearby stations is the same.

The difference in the temperature from top to bottom is itself a «causal factor» that drives the flow downward.

Not exact matches

To be honest, the emissions reductions from our power sector — in many ways the heart of the Paris Agreement — may not make much difference in achieving temperature stabilization in any event.

Our mushroom farms were in fact established on land reclaimed from a scrub forest zone never before subjected to cultivation with the major difference between day and night temperature necessary for the strongest, healthiest, tastiest fungus.

But somehow, perhaps because I'd only gotten home from vacations in Brazil a week a go — the difference between Brazil's always hot and humid climate and its tropical beaches and Buenos Aires» sudden drop in temperature just seems too stark too take in all at once.

Here in the mountains is very harsh climate: strong winds from the sea and the difference between daytime and night temperatures can be 30 ° C (from 40 ° to 10 °).

For example, a bacterium that finds its ways from contaminated water into the human body notices the difference in temperature.

Differences in the two structures analyses stem in part from the fact that at cryo - temperatures some flexible loops of the receptor appear more rigid than they are at room temperature.

Around 7.71 % of all deaths were caused by non-optimal temperatures, with substantial differences between countries, ranging from around 3 % in Thailand, Brazil, and Sweden to about 11 % in China, Italy, and Japan.

Travelling between the stars for a hundred light years or so, we would find ourselves moving between regions where the density of gas changes a millionfold — more extreme than the difference between air and water — and with changes in temperature from just a few degrees above absolute zero to over a million degrees.

We had expected milder weather than Barents experienced — in the «Little Ice Age», which lasted from 1450 to 1850, mean temperatures were between 1 and 2 °C colder than nowadays — but the difference in conditions was far greater than we had anticipated.

So when wind pulls warm water up from down deep, the temperature difference experienced at the interface of the water and ice can effectively submerse the glacier in a hot bath, with some areas experiencing more than a 10-fold increase in melt rate.

The team's research shows that in addition to contributions from natural forcings and global warming, temperature differences between the Atlantic and Pacific oceans play a role in causing drought and increasing wildfire risks.

This new research shows that in addition to a discernible contribution from natural forcings and human - induced global warming, the large - scale difference between Atlantic and Pacific ocean temperatures plays a fundamental role in causing droughts, and enhancing wildfire risks.

Researchers have determined that there is no appreciable difference in water nutrients, sunlight, water temperature or stratification from the time the blooms begin in November to the time they disappear in January.

The difference in seawater temperature from the long - term average is shown here as the event fizzled during May 2016.

The temperature difference between the Southern Great Plains and the Atlantic Ocean produces winds that carry moisture from the Gulf of Mexico to the Great Plains, according to a recent study in Nature Communications.

This difference in temperature creates a pressure gradient between the Rocky Mountains and the Atlantic Ocean that induces stronger winds that push moisture up from the Gulf of Mexico.

But in all images they saw variations of only 3 — 20 °C, instead of the kind of temperature difference they would expect from active lava flows.

A comparison between temperatures over the most recent available 30 - year period (1978 - 2007) shows high temperatures over parts of Russia (Figure below — upper left panel), and the difference between the GISTEMP and HadCRUT 3v shows a good agreement apart from around the Arctic rim and in some maritime sectors (upper right panel).

On the contrary, quantitative RT - PCR using the RNAs extracted from the MBs revealed that the difference in the Acks expression level in the MBs between the antennae - deprived and intact workers under high temperature was not statistically significant.

While there remain disparities among different tropospheric temperature trends estimated from satellite Microwave Sounding Unit (MSU and advanced MSU) measurements since 1979, and all likely still contain residual errors, estimates have been substantially improved (and data set differences reduced) through adjustments for issues of changing satellites, orbit decay and drift in local crossing time (i.e., diurnal cycle effects).

Hallelujah I am back in the real world and I am just saying that from a blogger perspective because if I was not a blogger needing my internet I would not be celebrating right now, seriously a 40 degree difference in temperature.

1B) Any difference in the difficulty in starting is going to vary far more with battery temperature and engine temperature than it will with a relatively insignificant draw from the devices you're adding.

With 755 horsepower the 2019 Chevrolet Corvette zr1 is the most powerful Corvette ever it's also the most technologically advanced behind me are the rolling s's at Road Atlanta and we're here to see if we can reach to the supercar levels of performance afforded by this thing's massive power big tires and the tall wing on the back after that we'll take to the streets to see if a car this powerful can behave itself in public this is a monster of a car I've had some brief track opportunities moving this morning to get used to the pace of this machine which is phenomenal we're gonna warm up as we get out to the road Atlanta and sort of build up to the pace that this car can operate at now initially when you hop in this car you have this shrine to the engine right above you you see the line of the hood it kind of dominates the center of the view you can see over it it doesn't affect visibility but it's immediately obvious and that kind of speaks to what makes this car special it's a monster of an engine listen to that [Music] that is tremendous tremendous acceleration and incredible power but what I finding so far my brief time here at the Atlanta is that everything else in the car is rut has risen to match hurt me while I lay into it on the back straight look you know 150 mile - an - hour indicated we're going to ease up a little bit on it because I need to focus on talking rather than driving but like I was saying the attributes of the rest of the car the steering the braking capability the grip every system of this car is riding to the same level of the power and I think that's what makes it really impressive initially this is undoubtedly a mega mega fast car but it's one that doesn't terrify you with its performance potential there's a level of electronic sophistication that is unparalleled at this price point but it's hard not to get you know totally slipped away by the power of this engine so that's why I keep coming back to it this car has an electronically controlled limited slip differential it has shocks filled with magnetically responsive fluid that can react faster to inputs and everything this car has a super sophisticated stability control system that teaches you how to drive it quick but also makes you go faster we haven't even gotten into exploring it yet because the limits of this car are so high that frankly it takes a while to grow into it but [Music] I think what's impressive about this car is despite how fast it is it is approachable you can buy this car to track dates with it and grow with it as a driver and as an owner I think that's a really special [Music] because you will never be more talented than this car is fast ever unless you are a racing driver casually grazing under 50 miles an hour on this straight okay I'm just going to enjoy driving this now [Music][Applause][Music] this particular Corvette zr1 comes with the cars track performance package a lot of those changes happen underneath the sheet metal but one of the big differences that is immediately obvious is this giant carbon fiber wing now the way this thing is mounted is actually into the structure of the vehicle and it makes you know loading the rear hatch a bit more difficult but we're assuming that's okay if you're looking for the track performance this thing delivers also giving you that performance are these Michelin Pilot Sport cup tires which are basically track oriented tires that you can drive on the street but as we wake our way to the front of the thing what really matters is what's under the hood that's right there's actually a hole in the hood of this thing and that's because this engine is so tall it's tall because it has a larger supercharger and a bunch of added cooling on it to help it you know keep at the right temperature the supercharger is way larger than the one on the zo six and it has a more cooling capacity and the downside is it's taller so it pops literally through the hood the cool thing is from the top you can actually see this shake when you're looking at it from you know a camera from the top of the vehicle this all makes for 755 horsepower making this the most powerful Corvette ever now what's important about that is this not just the power but likewise everything in the car has to be built to accommodate and be able to drive to the level of speed this thing can develop that's why you had the massive cooling so I had the aerodynamics and that's why I had the electronic sophistication inside [Applause] we had a lot of time to take this car on the track yesterday and I've had the night to think about things Matt today two crews on the road and see how this extreme performance machine deals with the sort of more civil minded stuff of street driving the track impressions remain this thing is unquestionably one of the most capable cars you can get from a dealer these days a lot of that's besides the point now because we're on the street we have speed limits they have the ever - present threat of law enforcement around every corner so the question is what does this car feel like in public when you slow this car down it feels like a more powerful Corvette you don't get much tram lining from these big wheels though we as the front end doesn't want to follow grooves in the pavement it is louder it is a little firmer but it's certainly livable on a day to day basis that's surprising for a vehicle of this capability normally these track oriented cars are so hardcore that you wouldn't want to drive them to the racetrack but let's face it you spend more time driving to the track than you do on the track and the fact that this thing works well in both disciplines is really impressive I can also dial everything back and cruise and not feel like I'm getting punished for driving a hardcore track machine that's a that's a really nice accomplishment that's something that you won't find in cars that are this fast and costs maybe double this much the engine in this car dominates the entire experience you can't miss the engine and the whole friend this car is sort of a shrine to it the way it pops out of the hood the way it's covered with coolers around the sides it is the experience of this car and that does make driving this thing special and also the fact that it doesn't look half bad either in fact I think it has some of the coolest looking wheels currently available on a new car this car as we mentioned this car has the track package the track package on this car gives you what they call competition bucket seats which are a little wide for my tastes but I'm you know not the widest person in the world this automatic transmission works well I mean there's so much torque again out of this engine that it can be very smooth and almost imperceptible its clunky on occasion I think I'd might opt for the manual although Chevy tells me about 80 % of its customers will go for the automatic I don't think they're gonna be disappointed and that's gonna be the faster transmission drag strip on the street - and on the racetrack man it was a little bit more satisfying to my taste though we've talked about the exhaust I have it set in the track setting let's quiet it down a little bit so you can hear the difference now I've set that separately from everything else so let's put it stealth what happened to the engine sound that's pretty that's pretty amazing man stealth is really stealth and then go back to track Wow actually a really big difference that's that's pretty great the Corvette has always been a strong value proposition and nowhere is that more evident than this zr1 giving you a nearly unbeatable track performance per dollar now the nice thing is on the road this doesn't feel like a ragged edge track machine either you could genuinely drive it every day the compromises are few and that's what makes this car so special if you like what you see keep it tuned right here and be sure to visit Edmunds.com [Music]

The carmaker explained that several factors can affect hybrid fuel economy more than regular gasoline engines, and among the differences highlighted were speed, as the difference between 75 mph and 65 mph can produce a 7 mpg difference in fuel economy; outside temperature, the difference between 40 °F and 70 °F can result in a 5 mpg difference; and vehicle break - in, the difference from 0 miles to 6,000 miles can be a 5 mpg difference.

When differences in scaling between previous studies are accounted for, the various current and previous estimates of NH mean surface temperature are largely consistent within uncertainties, despite the differences in methodology and mix of proxy data back to approximately A.D. 1000... Conclusions are less definitive for the SH and globe, which we attribute to larger uncertainties arising from the sparser available proxy data in the SH.

So to me the graphic is correct i.e. Corrections applied by GISS have increased the difference between the January 1910 and January 2000 temperature from 0.43 C in 2008 to 0.71 C in 2016.

So if I look at a trend from say just after WWII (largely bucket) to around 2000 (largely intake), there will be.3 degrees (assuming that is the difference) of warming attributable not to an actual temperature change, but to the switch in measurement method?

For instance, in your scenario of a 20 - yr temperature change of 0.3 ºC + / - 0.18 ºC, assuming a natural noise level (observed standard deviation of detrended annual global temperatures from 1977 - 2004) of 0.085 ºC, a statistically significant difference in the trend that leads to the lowest end of your range (a change of 0.12 ºC) and the trend that leads to the highest end of your range (0.48 ºC) doesn't begin to rise above the level of noise until around year 16 or 17.

Your calculation describes how much difference in infrared radiational heating, dQ, results from a given increment of temperature change, assuming emissivity and everything else remain fixed.

This presented a unique opportunity to study the effects... Comparing changes in the daily temperature range showed that the absence of dimming from aircraft pollution alone made a marked difference to the temperature.

Given that small difference you would have to have two boxes at the same time, not the same box at diffent times, cause normal variations in temperature from day to day would swamp your results.

It's the first plant plant of its kind in the states that generates electricity from the temperature differences in the ocean.

But in the data gaps, it consists of satellite data that have been converted to near - surface temperatures, where the difference between the two is determined by a kriging interpolation from the edges.

Before allowing the temperature to respond, we can consider the forcing at the tropopause (TRPP) and at TOA, both reductions in net upward fluxes (though at TOA, the net upward LW flux is simply the OLR); my point is that even without direct solar heating above the tropopause, the forcing at TOA can be less than the forcing at TRPP (as explained in detail for CO2 in my 348, but in general, it is possible to bring the net upward flux at TRPP toward zero but even with saturation at TOA, the nonzero skin temperature requires some nonzero net upward flux to remain — now it just depends on what the net fluxes were before we made the changes, and whether the proportionality of forcings at TRPP and TOA is similar if the effect has not approached saturation at TRPP); the forcing at TRPP is the forcing on the surface + troposphere, which they must warm up to balance, while the forcing difference between TOA and TRPP is the forcing on the stratosphere; if the forcing at TRPP is larger than at TOA, the stratosphere must cool, reducing outward fluxes from the stratosphere by the same total amount as the difference in forcings between TRPP and TOA.

That means saturation will not have occured; the OLR brightness temperature will be larger than the skin temperature, though the difference will be smaller for intensities in nearly horizontal directions — not just because the skin layer is colder but because some portion of the atmosphere below that is colder (the temperature will gradually approach the skin temperature going upward from the «photosphere» (effective emitting level) as you would call it in analogy with the sun).

Average July temperatures range from 2.4 °C to 3.6 °C on the south coast but notable differences in temperature occur with differences in terrain, and in the intermontane depressions, temperatures can reach 10 °C.

Based on the decrease in SO2 emissions in Europa, there should be a huge difference in temperature increase between less polluted areas and more polluted areas, downwind from the main sources.

The higher d18O values in the Wrangel tusks relative to the Jarkov mammoth and others from Siberia suggest considerably warmer temperatures and / or major differences in moisture transport during the middle Holocene relative to the late Pleistocene.»

The difference in radiant flux will be smaller between 222 K and 255 K, and larger between 288 K and 321 K, and it will take a greater GHE TOA forcing to reduce the effective radiating temperature (the temperature of a blackbody that would emit a radiative flux) at TOA from 288 K to 277 K as it would to reduce it from 277 K to 266 K, etc..

There are such large differences in the trends over these centuries both for temperature and for TSI (the only consistency is that the trends are all positive) that any attempt to analyse the influence from these data is hopeless.

since it is actually the TOTAL residence time of the energy as it is transported from ground to space that causes the difference in temperature.

Here we show that the hemispheric differences in temperature trends in the middle of the twentieth century stem largely from a rapid drop in Northern Hemisphere sea surface temperatures of about 0.3 6C between about 1968 and 1972.

Have you tried tracking the difference in the high temperature from the day before to the current days low temperature to demonstrate the change in the radiational cooling from one day to the next day?

We don't really know the magnitude of that lag as well as Barton implies we do, because it is very challenging to put CO2 records from ice cores on the same timescale as temperature records from those same ice cores, due to the time delay in trapping the atmosphere as the snow is compressed into ice (the ice at any time will always be younger older than the gas bubbles it encloses, and the age difference is inherently uncertain).

Weather often occurs as a result of differences in temperature and pressure from one place to another.

The mix of these diffusion coefficients gives rise to a dispersive rise in temperature that has subtle differences from the rise expected with a single - valued diffusion coefficient.