Sentences with phrase «such a long time scale»

And the good agreement for the past 700 years was quite a surprise to me — I did not expect these simple models to hold up for such a long time scale.

Yes and the real point about the inaccuracy of the GCMs is that natural + unconsidered variability in the outcome is so great and of such long time scale as to overstep the human time frame.

Not exact matches

If you're looking at such long time - scales, then normalizing to NGDP per capita would make a great deal of sense.

Satan did it, and fell... man, seduced by the father of lies, and lust for power has allowed pride to swell up in his heart, has done the same... Scriptures were written long ago, but we see them fulfilled with our own eyes (Dan.12: 4) There has never been time as such we're living in, when man is so advanced, yet the deprivation of human character on WORLDWIDE scale, is unprecedented from any time in history of mankind!

While the atmosphere is mainly causing climate variations on shorter time scales, from months to years, the longer - term fluctuations, such as those on decadal time scales, are primarily determined by the ocean.

Lead researcher Dr Morgan Beeby said: «We are used to observing evolution at the scale of animals or plants, such as the giraffe's neck slowly getting longer over time to reach previously inaccessible food.

The increased risk of further heat waves (intensive heat over relatively short time scales) as well as exposure to warmer temperatures over the longer term, suggest that recovery will depend on thermally - resistant individuals that may trade - off high temperature tolerance with other important attributes such as nutritional value or rapid growth.

Studies of modern, scaled - up programs that intend to impact long - term child development find, unlike the studies of small hothouse programs from the last century, that improvements in children's measurable skills and dispositions found at the end of participation in such programs usually fade away entirely by the time children are in the first few grades of elementary school.

«This is a challenging time of initiating such a change movement,» says Massachusetts education secretary Paul Reville, referring to the economic downturn, «but the cost of not initiating this scope and scale of change far exceeds in the long run the cost of doing it.»

- the game's shading mechanism has changed, which allows for increased gear texture quality - all graphical aspects and programming mechanisms have been built up from scratch for this sequel - maximum resolution is 1080p in TV mode - a bigger focus for Nintendo was the 60 frames per second - occasionally the resolution will be scaled down when there is too much ink displaying on the screen - Nintendo reduced the CPU load and refined the way to use CPU power effectively to maintain 60 fps in all matches - weapons were tweaked to let players be more creative by thinking about unique weapon characteristics and their best uses - weapons are designed to be effective when they are used during the right occasion - Special weapons are stronger than the original ones when used in the right situation, but weaker otherwise - the damage and effect of slowing down your movement when you step in the opponent's ink are reduced from original - you can jump up in rank if you're good enough, but only up until S - you can't jump up from C, B or A to S + - when you win battles in Ranked mode, the Ranked meter fills and your rank goes up when its fully filled - when you lose a battle, the gauge does not decrease, but the meter starts to crack - once the meter reaches its limit, it breaks - when the meter breaks, you have to start over again from the beginning or from a lower rank - highest rank is still S +, but if you fill up the Ranked meter, you get numbers after the alphabet such as «S +1», «S +2» and so on - maximum number is «S +50», but this number will not be displayed to your opponent - you are the only one to see it, and you can check it on your own status screen - Ranked Power is calculated by an algorithm to measure how strong each player is with minuteness - this will determine if a player's rank is worthy of receiving a big jump (like from «C» to «A»)- Ranked Power has no relation to your splat rate, and is more tied into to how well you lead your team to victory - you won't drop off more than one rank even if you play poorly - stage rotation time was changed to two hours - this was done because the devs expected people to play for an hour or so, but they found people play much longer - with Salmon Run, Nintendo considered how to implement a co-op oriented mode in a player - versus - player type of game - the devs will monitor how users are playing this mode to see if there's some tweaks they can throw in - more Salmon Run maps will be added in the future, but Nintendo wouldn't comment on adding more enemy types to the mode - rewards are changed each time Salmon Run is played - you can obtain rewards when playing locally, but not gear - originally Nintendo had an idea for this mode, but had no background setting, enemy designs, etc. - Inoue suggested that it should be salmon - themed - when Nintendo hosted the Splatfest that pit Callie against Marie, the development of Splatoon 2 had started - the devs had already decided to have the result reflected in the sequel - they even had an idea to announce the Splatfest with a phrase «Your choice will change the next Splatoon» - the timing to announce a sequel wasn't right, so they decided against this - they eventually released a series of short stories about the Squid Sisters to show how the Splatfest affected the sequel's story - Nintendo wouldn't say if Marina is an Octoling, and noted that Inklings are not paying attention to this too much - Inklings don't care about appearances, as long as everyone is doing something fresh - the Squid Sisters had composers who produced their songs, but Off the Hook are composing their music by themselves - Pearl is genius artist, but she couldn't find a right partner because she's a bit too edgy - she eventually found Marina as a partner though, and their chemistry is sparkling right now - Nintendo is planning a year of content updates for Splatoon 2 - when finished, the quantity of stages will be more than the original - some of the additional stages are totally new and some will be arranged stages from the first game - not all original stages will return and they are choosing stages based on the potential for them to be improved - Brella is shotgun-esque weapon, so the ink hits your opponent more if you are closer - it can shield damage when you open it, but the amount of damage has a limit and once it reaches it, it breaks - you can shoot ink, but you can't use the shield feature when it breaks - the shield won't prevent your allies ink - there are more new weapon categories which haven't been revealed yet - there are no other ranked modes outside of the three current options - the future holds any sort of possibility, but the devs didn't get specific about adding more content like that - for the modes, they adjusted the rule designs so that players will experience the more interesting aspects

Magnetic Fields features early - and later - career works, pieces from specific series, several exhibited for the first time, and the long - awaited reappearance of iconic works such as Mavis Pusey's large - scale painting Dejygea (1970) from the Whitney Museum of American Art's 1971 exhibition Contemporary Black Artists in America.

Magnetic Fields features a range of works, including early and later career examples, several exhibited for the first time, and the long - awaited reappearance of iconic works such as Mavis Pusey's large - scale painting Dejyqea (1970), featured in the Whitney Museum of American Art's landmark 1971 exhibition Contemporary Black Artists in America.

For variability on a long time scale, the effect is generally constant over a short time period (such as Milankovitch cycles).

If we decide, as Lomborg suggests, to focus exclusively on a handful of top priorities at the expense of all others, especially those that are more complex and operate over longer time scales, such as Climate Change, we are doing little more than arranging the Titanic's proverbial deck - chairs.

I did a simple calculation on a time scale of several centuries, and only the Sun has such long range variability.

On longer time - scales, integrated weather patterns regulate biological processes such as the timing of leaf emergence or excision, uptake of nitrogen by autotrophs, and rates of organic soil decay and turnover of inorganic nitrogen.

If this forecast is correct, it will take a long time or big technological innovations on the production side to induce large - scale fossil - fuel production from high - cost areas such as the Arctic Ocean, regardless of sea - ice conditions.

Although such approaches provide important spatial coverage of long - term trends, their accuracy will be difficult to assess unless seasonal and interannual time scales of pH variability can be adequately resolved.»

The 20 - year horizon is relevant to short - term impacts, such as changes in weather patterns; the 100 - year horizon applies to longer time - scale changes, such as sea - level rise; while 500 years represents the longest time - scale it is felt reasonable to consider given our current knowledge.

The long time range of this dataset allows scientists to examine better long time scale climate processes such as the Pacific Decadal Oscillation and the Atlantic Multidecadal Oscillation as well as looking at the dynamics of historical climate and weather events.

Smaller - scale deployments have occurred at a variety of locations, particularly such well - studied sites as the University of Hawai`i at Mānoa's Hawaii Ocean Time - series (HOT) station, where long biogeochemical records from floats (Figure 1) can be calibrated against shipboard measurements.

It appears we agree on the inability of the global models to simulate the natural variations on decadal and, presumably longer time scales, of large scale circulation patterns such as ENSO, the PDO, the NAO etc..

The main difference between H2O and CO2 (apart from the numerical differences of their specific physical properites such as degree of freedom, thermal capacity, physical mass, etc) in terms of their effects on the atmosphere is that water is capable of condensing into liquid to form clouds and readily and rapidly moves between surface and atmosphere, daily, seasonally, annually and on even greater time scales, but CO2 does not liquify in the biosphere and transfers over mostly long time periods between surface (primarily oceans, seas, etc) and the atmosphere.

The long time scale for this recovery arises because ozone depleting gases such as chlorofluorocarbons are only removed from the atmosphere by natural processes at very slow rates.

Physically, C1 can be thought of as representing the concentration of CO2 in long - term stores such as the deep ocean; C1 + C2 as representing the CO2 concentration in medium - term stores such as the thermocline and the long - term soil - carbon storage; and C = C1 + C2 + C3 as the concentration of CO2 in those sinks that are also in equilibrium with the atmosphere on time scales of a year or less, including the mixed layer, the atmosphere itself and rapid - response biospheric stores.

Recent work (e.g., Hurrell 1995, 1996; Thompson and Wallace 1998; Corti et al., 1999) has suggested that the observed warming over the last few decades may be manifest as a change in frequency of these naturally preferred patterns (Chapters 2 and 7) and there is now considerable interest in testing the ability of climate models to simulate such weather regimes (Chapter 8) and to see whether the greenhouse gas forced runs suggest shifts in the residence time or transitions between such regimes on long time - scales.

Such changes might depend on a social movement for climate stabilization that supports long - term changes in social norms (e.g. about family size), greater availability of mass transit, climate - friendly urban design, or other actions that are impractical on the short term but on a longer time scale increase the plasticity of potentially high - impact behaviors.

The time scales for other end - use infrastructure (e.g. processes, building stock, roads and rail) may be even longer, though components (such as heaters, cars) may have considerably faster turnover.

The net effect of such compensations is that averages over larger areas or longer time scales commonly will give smaller estimates of change.

229 Time resolution on the scale of a year or two can be obtained from semi-fossil trees, e.g., Roig et al (2001) have a 1229 - year - long stretch of tree - ring widths from the middle of the last ice age at 40 ° S that shows abrupt droughts with abrupt recoveries (tenfold changes in yearly accumulation), but they are floating in absolute time and such local records can not yet be matched to events in the ice - core recoTime resolution on the scale of a year or two can be obtained from semi-fossil trees, e.g., Roig et al (2001) have a 1229 - year - long stretch of tree - ring widths from the middle of the last ice age at 40 ° S that shows abrupt droughts with abrupt recoveries (tenfold changes in yearly accumulation), but they are floating in absolute time and such local records can not yet be matched to events in the ice - core recotime and such local records can not yet be matched to events in the ice - core records.

In looking at longer time scales, major shifts in climate such as the ice ages are easily recognizable, and viewing a long - term data set can provide the observer with a sense of the «big picture» of the climatic trends.

Thus there are primarily internal system changes forcing climate responses, not primarily external such as the absolute value of solar power (except over much longer time scales).

This inconsistency between model results and observations could arise either becaise «real world» amplification effects on short and long term time scales are controlled by different physical mechanisms, and models fail to capture such behavior, or because non-climatic influences remaining in some or all of the observed tropospheric datasets lead to biased long - term trends, or a combination of these factors.

Climate threshold - The point at which external forcing of the climate system, such as the increasing atmospheric concentration of heat - trapping gases (greenhouse gas es), triggers a significant climatic or environmental event which is considered unalterable, or recoverable only on very long time - scales, such as widespread bleaching of corals or a collapse of oceanic circulation systems.

By the way, we also did a paper on millennial - scale solar geoengineering (Cao et al, 2016) showing that, in at least one climate model, solar geoengineering behaves quite well on the 1000 - year time scale with no substantial long term growth in climate change as ocean circulation and such adjusts to the new conditions.

The glacial - interglacial cycles are an example of tight coupling between climate and the carbon cycle over long time scales, but there is also clear evidence of the carbon cycle responding to short - term climatic anomalies such as the El Niño - Southern Oscillation (ENSO) and Arctic Oscillation (Rayner et al., 1999; Bousquet et al., 2000; C. Jones et al., 2001; Lintner, 2002; Russell and Wallace, 2004) and the climate perturbation arising from the Mt. Pinatubo volcanic eruption (Jones and Cox, 2001a; Lucht et al., 2002; Angert et al., 2004).

Such a change is irreversible if the recovery time scale due to natural processes is significantly longer than the time it took to reach the new state.

Climate is individual weather observations / predictions integrated over time and area, taking longer - scale trends into account and allowing us to identify such trends.

Other components of the climate system, such as the ocean and the large ice sheets, tend to operate on longer time scales.

«However, it is less common to observe such a large - scale campaign go relatively unnoticed for such a long period of time.

It is challenging to imagine ineptitude at such a grandiose scale, so the logical alternative is that they had been aware of the issue for a long time and voluntarily chose to hide this information from their investors and the public at large.

Although some view a small block - size limit increase as nothing more than «kicking the can down the road,» the reality is that more time is needed to fully develop long - term solutions, such as the Lightning Network or flexcap, that could help Bitcoin scale to millions (or even billions) of users over time.

The Incope (Bodenmann, 2000) is a questionnaire (5 - point scale) with 23 items (α = 0.80) developed on the basis of the COPE (Carver, Scheier, & Weintraub, 1989) measuring the following subscales such as active problem - solving («I attempt to tackle and solve the problem»), positive self - verbalization («I persuade myself that I will make it»), rumination («I ruminate for a long time and keep on thinking about the occurrence»), passivity / evasion («I wait until things change on their own, even if I might be able to do something»), negative emotional expression («I express my feelings without considering what this means for others»), substance use («I consume something that calms me down (cigarettes, alcohol, sweets, tranquiliser»)(α = 0.52 to α = 0.80).