Sentences with phrase «over long time scales in»

Not exact matches

The time scale over which an investor will obtain feedback from a seed stage investment is the longest in the venture capital business.

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The fish's scale captures systemic cortisol exposure over longer periods of time making it suitable to quantify chronic stress in fish.

Countering a widely - held view that thawing permafrost accelerates atmospheric warming, a study published this week in the scientific journal Nature suggests arctic thermokarst lakes are «net climate coolers» when observed over longer, millennial, time scales.

The geological search for ancient life frequently zeroes in on fossilized organic structures or biominerals that can serve as «biosignatures,» that survive in the rock record over extremely long time scales.

Through crowdsourcing — an open call for voluntary assistance from a large group of individuals — Americans can study and tackle complex challenges by conducting research at large geographic scales and over long periods of time in ways that professional scientists working alone can not easily duplicate.

While this leads to an elevation in the level of scientific understanding from very low in the TAR to low in this assessment, uncertainties remain large because of the lack of direct observations and incomplete understanding of solar variability mechanisms over long time scales.»

For significant periods of time, the reconstructed large - scale changes in the North Pacific SLP field described here and by construction the long - term decline in Hawaiian winter rainfall are broadly consistent with long - term changes in tropical Pacific sea surface temperature (SST) based on ENSO reconstructions documented in several other studies, particularly over the last two centuries.

We are very impressed by Fred Kavli's design of these new awards, which span from the very grand scale of astrophysics to the microscopic level of nanotechnology, and to the level in between: the brain - no doubt the most complex organ created by the biological evolution over a very, very long time... billions of years.

In fact, over long time scales, just not bothering to re-balance tends to allow the equities to take over and have an increasingly similar effect -:)

- 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

The silver lining i see here is invaluable experience creating and managing projects of the size and scale o XcX... The evolution of a long long long overdue open world design that finally does nt rely on «potato world» land / space / time compression (the hardware technology has been capable for over a decade...) This experience seems to have paid off in spades with monolithsofts work on the new Zelda being a clear show stopper.

There are of course other causes for other changes that have occurred, including suspected asteroid impacts, changes in volcanism over the eons which can lead to the buildup or reduction of greenhouse gases over long time scales, etc..

The Earth's rotation and position change in cycles in various ways over long time scales.

But over that long a time scale, they are much more a matter of choice, and less a matter of the inertia in the current infrastructure.

Back in 2001, Peter Doran and colleagues wrote a paper about the Dry Valleys long term ecosystem responses to climate change, in which they had a section discussing temperature trends over the previous couple of decades (not the 50 years time scale being discussed this week).

Over even longer time scales (hundreds of years) there are a number of paleo - records that correlate with records of cosmogenic isotopes (particularly 10Be and 14C), however, these records are somewhat modulated by climate processes themselves (the carbon cycle in the case of 14C, aerosol deposition and transport processes for 10Be) and so don't offer an absolutely clean attribution.

While this leads to an elevation in the level of scientific understanding from very low in the TAR to low in this assessment, uncertainties remain large because of the lack of direct observations and incomplete understanding of solar variability mechanisms over long time scales.»

Over long term time scales I see a smaller global population of maybe 3 billions, living in cities but with low rise passive solar design homes and offices.

But this human adaptation time scale may be longer than the time over which climate change affects storms, so that comparatively small changes in the frequency of generational events can have large social consequences.

Both are at different time scales, where any (theoretical) influence of CO2 need to change the ocean temperatures over a sufficient long period (10 - 30 years), to be visible in the statistics.

Global Temperature is an example of a bulk property, and it does indeed average out over sufficient time scales; hence showing that whatever chaos, spatio - temporal or otherwise, is present in the system on short timescales it does not affect our longer term predictions.

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.

It doesn't mean that there can't be any natural variability that appears as wobbles in the temperature record (or in other climate variables), masking the multi-decadal temperature trend over a time scale shorter than 20 years with the effect that the longer term trend is not statistically detectable in the time series, if one chooses the time period only short enough.

Jan Perlwitz says:» It doesn't mean that there can't be any natural variability that appears as wobbles in the temperature record (or in other climate variables), masking the multi-decadal temperature trend over a time scale shorter than 20 years with the effect that the longer term trend is not statistically detectable in the time series, if one chooses the time period only short enough.»

I'm very convinced that the physical process of global warming is continuing, which appears as a statistically significant increase of the global surface and tropospheric temperature anomaly over a time scale of about 20 years and longer and also as trends in other climate variables (e.g., global ocean heat content increase, Arctic and Antarctic ice decrease, mountain glacier decrease on average and others), and I don't see any scientific evidence according to which this trend has been broken, recently.

This places recent global warming trends in the context of temperature changes over longer time scales.

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.

1) You suggested that photosynthesis was inappropriately ignored in K&T's diagram (which by definition gives global averages over long time - scales).

The variations over time depicted for the various datasets are in generally good agreement, notwithstanding differences in absolute amounts, but there are differences on the longest time scales that are prominent for some regions.

On longer time - scales, and over the majority of large ocean regions in the 20th century, there is good agreement between NMAT and SST.

«What we're going to be doing next is trying to understand more about the relationships between the proxies that we measured in the mosses, how they've changed over longer time scales, before the advent of the human influence on climate,» Dr. Amesbury revealed.

If a scientist and in particular climate scientists don't understand the wide swings that do occur in data over short multidecadal time scales then how can they be trusted with understanding the large climatic swings on longer millenia time scales or vise - versa.

If you're interested in a solar electric system for your home and you live in a state with good incentives, it's always a better idea to act sooner rather than later — programs run out of funding, are designed to scale back over time, or reach their megawatt - capacity goals eventually, and if you wait too long you might find yourself stuck without access to those funds.

Forecasts over any longer time scales are in the fantasy realm of BBQ summers.

The sensitivity he then derives is projected back using the 0.8 deg C warming over the 20th C. However, this is ludicrous — the sensitivity in the recent period can't be more than say, 1 ppmv per 0.1 deg C. Projected back you would have say a 10 ppmv (max) change over the 20th C. Paleo - climate constraints demonstrate that CC feedback even on really long time scales is not more than 100 ppmv / 6 deg C (i.e. 16 ppmv / deg C), and over shorter time periods (i.e. Frank et al, 2010) it is more like 10 ppmv / deg C. Salby's sensitivity appears to be 10 times too large.

Or to put it another way, there is no reason to expect global mean temp to be linearly related to CO2 forcing, when all sorts of other things have changed in nonlinear fashion over these long time scales.

It is only urban records that are available in many regions of the world to provide what BEST calls «regional expectations» over century - long time scales.

Heat diffusion and permafrost melting takes time — in fact, the deeper Arctic permafrost can be seen as a relic of the last glaciation, which is still slowly eroding — so any significant loss of permafrost soil carbon will happen over long time scales.

The red areas are places to be flooded with 1 meter sea level rise (all but certain by 2100); the yellow areas are with 6 meters of sea level rise (which would happen over a longer time scale for sure, but is still worth considering as something which we are collectively setting in motion).

I have broad training in both atmospheric science and oceanography, and I am particularly interested in coupled atmosphere - ocean climate dynamics over long time scales.

We looked at volcanoes, solar effects, CO2 etc. and while we found clear signals (increasing + ve phase in each case), the signals are small compared to the huge interannual variability, and are thus only detectable with many examples superposed, or over long time scales.