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 winter
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 winter
different 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.