Sentences with phrase «different amount of warm»

Every person needs a different amount of warm up, but everyone needs a longer warm up in cold weather.
Regarding the effects of different amounts of warming, I'm reminded of a quotation by Prof Kevin Anderson.
One direction is to see what happened in the far past with different amounts of warming.
There is uncertainty in the climate sensitivity of the Earth and in the response of the carbon cycle, and the papers are extremely useful in the way that they propagate these uncertainties to the probabilities of different amounts of warming.
The oceans have a vertical temperature profile, they have accumulated huge amounts of energy over the last half - century of measurements, that translates into different amounts of warming over the vertical ocean profile.

Not exact matches

You adjust the heat for different size bottles and jars by the amount of water you put into the warming chamber.
The typology includes logical problems, algorithmic problems, story problems (which have underlying algorithms with a story wrapper that amounts to an algorithmic problem), rule - using problems, decision - making problems (e.g., cost - benefit analysis), troubleshooting (systematically diagnosing a fault and eliminating a problem space), diagnosis - solution problems (characteristic of medical school and involving small groups understanding the problem, researching different possible causes, generating hypotheses, performing diagnostic tests, and monitoring a treatment to restore a goal state), strategic performance, case analysis (characteristic of law or business school and involving adapting tactics to support an overall strategy and reflecting on authentic situations), design problems, and dilemmas (such as global warming, which are complex and involve competing values and which may have no obvious solutions).
Re my 441 — competing bands — To clarify, the absorption of each band adds to a warming effect of the surface + troposphere; given those temperatures, there are different equilibrium profiles of the stratosphere (and different radiative heating and cooling rates in the troposphere, etc.) for different amounts of absorption at different wavelengths; the bands with absorption «pull» on the temperature profile toward their equilibria; disequilibrium at individual bands is balanced over the whole spectrum (with zero net LW cooling, or net LW cooling that balances convective and solar heating).
The Global Footprint Network (GFN) has developed the concepts of biocapacity — the amount of land available to provide for human needs, and ecological footprint — the land needed to satisfy the consumption of different nations in a sustainable manner, including the biological capacity to absorb and mitigate the carbon dioxide emissions that lead to global warming.
This graph shows the equivalent amount of human induced global warming attributed to the different gases.
Because of the different heat capacity of the oceans and the atmosphere — the amount of energy which would heat the atmosphere by 1 K (Kelvin) will only heat the oceans by 0.001 K. Any lack of warming of the troposphere can be excused by a minuscule change in ocean temperature.
The surface warming is also consistent with the many physical indicators, and the observed amount of warming is consistent with the expected range of climate sensitivity, which itself is based upon many different lines of evidence.
This slower warming of the tropical Pacific induces changes in the atmospheric circulation that can be seen in the reanalyses, but two different reanalysis products that incorporate different amounts of satellite data in different ways produce conflicting estimates of the change in circulation.
The results presented here contribute to our understanding of the likely range under different amounts of global mean warming.
Different parts of the planet may have since warmed by different amounts, but they certainly all warmed or San Franciscans would have been able to skate on the San Francisco Bay in the winterDifferent parts of the planet may have since warmed by different amounts, but they certainly all warmed or San Franciscans would have been able to skate on the San Francisco Bay in the winterdifferent amounts, but they certainly all warmed or San Franciscans would have been able to skate on the San Francisco Bay in the winter of 1905.
The age of melting ice at the different ice caps will be dependent on their slope, aspect and situation, which will affect the amount of ice accumulated during the late Holocene and the melt rate in the current warm period.
It is remarkable that two areas of ocean so near to each other warmed by such different amounts.
The amount of adjustments to global temperature data is odd shall we say, HADCRUt4 showing different (warmer) than HADCRUT3 for example.
The main curiosity about these, other than the wide variety of amounts of warming, is the different timing of the warming
Knowing the different formation mechanisms will help scientists predict the amount of water vapor in the upper atmosphere, which affects the balance of warming and cooling that determines the Earth's climate change.
Are you claiming that if the atmosphere were replaced with a different set of gasses that do not contain GHG molecules, but still had all the other macro effects such as clouds etc in the exact same amount as our current atmosphere... are you claiming that this atmosphere would NOT cause (directly or indirectly) the surface of the earth to warm at all?
The elements are: (1) the amount of temperaturechange since 1850; (2) whether the change is in the range of natural variability or is attributable to humans; (3) the amount of warming that greenhouse gases (CO2 and equivalents) will warm the Earth in the future; and whether for the most likely scenarios, there are more losers than winners and if the change is just different.
Berkeley Lab researchers Dev Millstein and Surabi Menon found that atmospheric feedback — such as changes in cloud cover or precipitation — does have an important effect, resulting in different amounts of cooling in different cities, but that cool roofs and pavements are still beneficial for combating global warming.
Science writer Greg Laden wrote that the Duke study will receive «criticism from climate scientists» because it includes language that suggests it is assessing the likelihood of different warming scenarios by predicting the amount of greenhouse gas emissions that will occur in the future, which it can't possibly know.
Tau doesn't tell him what he wants to know; he has written at least one post on papers which show that adding the same quantity of water vapor to the atmosphere at different altitudes creates different amounts of radiative forcing: https://scienceofdoom.com/2010/09/18/clouds-and-water-vapor-part-three/ So tau can be the same and the temperature profile of the atmosphere can be the same, but warming will be different.
To make their predictions, Peng's team analyzed three different models of warming — and the least amount of warming effectively triples the impact of the heat waves we're seeing now.
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