Sentences with phrase «temperature changes in the context»

Indirect estimates of temperature change from such sources as tree rings and ice cores help to place recent temperature changes in the context of the past.

Not exact matches

«This Agreement, in enhancing the implementation of the [2015 United Nations Framework Convention on Climate Change], including its objective, aims to strengthen the global response to the threat of climate change, in the context of sustainable development and efforts to eradicate poverty, including by: (a) Holding the increase in the global average temperature to well below 2 °C above pre-industrial levels and pursuing efforts to limit the temperature increase to 1.5 °C above pre-industrial levels, recognizing that this would significantly reduce the risks and impacts of climate change; (b) Increasing the ability to adapt to the adverse impacts of climate change and foster climate resilience and low greenhouse gas emissions development, in a manner that does not threaten food production; and (c) Making finance flows consistent with a pathway towards low greenhouse gas emissions and climate - resilient develoChange], including its objective, aims to strengthen the global response to the threat of climate change, in the context of sustainable development and efforts to eradicate poverty, including by: (a) Holding the increase in the global average temperature to well below 2 °C above pre-industrial levels and pursuing efforts to limit the temperature increase to 1.5 °C above pre-industrial levels, recognizing that this would significantly reduce the risks and impacts of climate change; (b) Increasing the ability to adapt to the adverse impacts of climate change and foster climate resilience and low greenhouse gas emissions development, in a manner that does not threaten food production; and (c) Making finance flows consistent with a pathway towards low greenhouse gas emissions and climate - resilient develochange, in the context of sustainable development and efforts to eradicate poverty, including by: (a) Holding the increase in the global average temperature to well below 2 °C above pre-industrial levels and pursuing efforts to limit the temperature increase to 1.5 °C above pre-industrial levels, recognizing that this would significantly reduce the risks and impacts of climate change; (b) Increasing the ability to adapt to the adverse impacts of climate change and foster climate resilience and low greenhouse gas emissions development, in a manner that does not threaten food production; and (c) Making finance flows consistent with a pathway towards low greenhouse gas emissions and climate - resilient develochange; (b) Increasing the ability to adapt to the adverse impacts of climate change and foster climate resilience and low greenhouse gas emissions development, in a manner that does not threaten food production; and (c) Making finance flows consistent with a pathway towards low greenhouse gas emissions and climate - resilient develochange and foster climate resilience and low greenhouse gas emissions development, in a manner that does not threaten food production; and (c) Making finance flows consistent with a pathway towards low greenhouse gas emissions and climate - resilient development.

Now in its 25th year, the report pulls together hundreds of scientists from dozens of countries to piece together the changes from the previous year in all aspects of the Earth's climate — from carbon dioxide levels to the planet's rising temperature, from glacier melt to change in soil moisture — and puts them in the context of decades - long trends.

It's a luxury to revisit whatever is universal from the original and to find a new vehicle for that universality in this new context which is a very sadly special context because the world has changed so much, and Trump is in power and the temperature is very specific and very different and the story becomes very urgent.

(Here dS = change in entropy, T = temperature, dQ is the change in heat context).

First, for changing just CO2 forcing (or CH4, etc, or for a non-GHE forcing, such as a change in incident solar radiation, volcanic aerosols, etc.), there will be other GHE radiative «forcings» (feedbacks, though in the context of measuring their radiative effect, they can be described as having radiative forcings of x W / m2 per change in surface T), such as water vapor feedback, LW cloud feedback, and also, because GHE depends on the vertical temperature distribution, the lapse rate feedback (this generally refers to the tropospheric lapse rate, though changes in the position of the tropopause and changes in the stratospheric temperature could also be considered lapse - rate feedbacks for forcing at TOA; forcing at the tropopause with stratospheric adjustment takes some of that into account; sensitivity to forcing at the tropopause with stratospheric adjustment will generally be different from sensitivity to forcing without stratospheric adjustment and both will generally be different from forcing at TOA before stratospheric adjustment; forcing at TOA after stratospehric adjustment is identical to forcing at the tropopause after stratospheric adjustment).

Also to help with context what is the average and standard deviation of the change in temperature from one year to the next?

He argued that averages of the Earth's temperature are devoid of a physical context which would indicate how they should be interpreted or what meaning can be attached to changes in global temperatures.

In this context, it is refreshing to see a new paper at the National Bureau of Economic Research by Alan Barreca et al., titled, «Adapting to Climate Change: The Remarkable Decline in the U.S. Temperature - Mortality Relationship over the 20th Century.&raquIn this context, it is refreshing to see a new paper at the National Bureau of Economic Research by Alan Barreca et al., titled, «Adapting to Climate Change: The Remarkable Decline in the U.S. Temperature - Mortality Relationship over the 20th Century.&raquin the U.S. Temperature - Mortality Relationship over the 20th Century.»

Fewer models have simulated tropical cyclones in the context of climate change than those simulating temperature and precipitation changes and sea level rise, mainly because of the computational burden associated with the high resolution needed to capture the characteristics of tropical cyclones.

Sea surface temperature (SST) measured from Earth Observation Satellites in considerable spatial detail and at high frequency, is increasingly required for use in the context of operational monitoring and forecasting of the ocean, for assimilation into coupled ocean - atmosphere model systems and for applications in short - term numerical weather prediction and longer term climate change detection.

In fact, they may do so more efficiently than more uniform temperature change; warming one hemisphere with respect to the other is an excellent way of pulling monsoonal circulations and oceanic ITCZs towards the warm hemisphere (the last few years have seen numerous studies of this response, relevant for ice ages and aerosol forcing as well as the response to high latitude internal variability; Chiang and Bitz, 2005 is one of the first to discuss this, in the ice age context; I'll try to return to this topic in a future postIn fact, they may do so more efficiently than more uniform temperature change; warming one hemisphere with respect to the other is an excellent way of pulling monsoonal circulations and oceanic ITCZs towards the warm hemisphere (the last few years have seen numerous studies of this response, relevant for ice ages and aerosol forcing as well as the response to high latitude internal variability; Chiang and Bitz, 2005 is one of the first to discuss this, in the ice age context; I'll try to return to this topic in a future postin the ice age context; I'll try to return to this topic in a future postin a future post.)

This page is designed to provide a simple, convenient tool for people to observe temperature trends since weather records began in Western Australia, particularly in the context of perceived climate change.

This change in sea level occurred in the context of different orbital forcing and with high latitude surface temperature, averaged over several thousand years, at least 2 °C warmer than present.

In this context «natural variability» seems to be a catchphrase for unknown forcings and feedbacks that change global temperature in ways that we can't predict or quantifIn this context «natural variability» seems to be a catchphrase for unknown forcings and feedbacks that change global temperature in ways that we can't predict or quantifin ways that we can't predict or quantify.

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

In most cases, these range from about 2 to 4.5 C per doubled CO2 within the context of our current climate — with a most likely value between 2 and 3 C. On the other hand, chapter 9 describes attempts ranging far back into paleoclimatology to relate forcings to temperature change, sometimes directly (with all the attendant uncertainties), and more often by adjusting model parameters to determine the climate sensitivity ranges that allow the models to best simulate data from the past — e.g., the Last Glacial Maximum (LGM).

If you're talking about a change in the rate, trend of warming, or even just say that «warming has slowed» in the context of the general discussion about global temperature records, you are implying something about a change in trend.

Adaptation (Art. 7)-- The Paris Agreement establishes a global goal on adaptation — of enhancing adaptive capacity, strengthening resilience and reducing vulnerability to climate change in the context of the temperature goal of the Agreement.

Viewed in context, the record temperatures underscore the undeniable fact that we are witnessing, before our eyes, the effects of human - caused climate change.

I brought this up in the context that this is exactly the kind of linear relationship claimed between forcing and temperature in the climate, where the change in the output variable, global temperature, is claimed to be a certain number λ times the change in the input variable, forcing.

The workshop was organized to allow participants to take a global perspective and consider the influence of the Arctic in the context of forcing from other components of the climate system, such as changes in the tropics, ocean circulation, and mid-latitude sea surface temperature.

To be useful in a risk context, climate change assessments therefore need a much more thorough exploration of the tails of the distributions of physical variables such as sea level rise, temperature, and precipitation, where our scientific knowledge base is less complete, and where sophisticated climate models are less helpful.

Just for one prominent example, when NOAA and / or NASA cite 2014 as being the hottest year on record, in a context of stating their official positions concerning climate change — as were 1998, 2005, and 2010 similarly cited — then for purposes of verifying the AR5 model ensemble, what they are really saying is that the trend of peak hottest years is what matters most to them as climate scientists, not the central trend of observed temperatures.

In context, the statement relates to Jones» research on changes in global temperaturIn context, the statement relates to Jones» research on changes in global temperaturin global temperature.

«In the context of climate change, we can say that, in north India, the temperature is increasing more compared to south IndiIn the context of climate change, we can say that, in north India, the temperature is increasing more compared to south Indiin north India, the temperature is increasing more compared to south India.

Nor in a Southern Hemisphere context are «atmospheric circulation changes» independent of temperature changes: changes in temperature are invariably associated with atmospheric circulation changes, particularly with movements of the southern westerlies towards and away from the equator.

In the context of the climate system, if you are saying that atmospheric concentrations of GHGs build at an exponential rate against linear changes in temperature, indeed, we must accept hypothesis In the context of the climate system, if you are saying that atmospheric concentrations of GHGs build at an exponential rate against linear changes in temperature, indeed, we must accept hypothesis in temperature, indeed, we must accept hypothesis A.

Giaever does not seem to know how to put the observed 0.8 °C global surface temperature change in proper context.

Radiative feedbacks act the same way as radiative forcings, except that they themselves are dependent on temperature changes (the distinction depends on timescale and context; also, in some contexts the feedbacks» effects are described as radiative forcings — for example, the radiative forcing of the increase in water vapor that would occur for a given temperature increase).

That +0.29 °C temperature since 1988 change took place in a global climate context that included not only the impact of multiple powerful El Niños, but also an atmosphere that was infused from 1989 - 2016 with over 50 % of the total human CO2 emissions (metric tonnes) emitted since 1850.

To achieve the ultimate objective of the Convention to stabilize greenhouse gas concentration in the atmosphere at a level that would prevent dangerous anthropogenic interference with the climate system, we shall, recognizing the scientific view that the increase in global temperature below 2 degrees, on the basis of equity and in the context of sustainable development, enhance our long - term cooperative action to combat climate change.

«They surround us everyday in a variety of contexts, and a great example that we are all very familiar with is the diurnal cycle, day and night temperature changes.