Sentences with phrase «net global response»

They indicate that some regions of the Earth's surface may cool, and others warm, by amplitudes larger than the net global response, as a result of differences in solar heating of land and ocean surfaces.

Not exact matches

Climate scientists would say in response that changes in ocean circulation can't sustain a net change in global temperature over such a long period (ENSO for example might raise or lower global temperature on a timescale of one or two years, but over decades there would be roughly zero net change).
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The equilibrium response to an addition of RF at a level is an increase in net upward flux consisting of LW radiation (the Planck response, PR) plus a convective flux response CR; CR is approximately zero at and above the tropopause in the global time average.
Since it is difficult to understand what exactly is meant by Holistic Management ® in this context, and there is no scientific literature that we are aware of that supports a significant net gain of soil carbon across environments in response to his method, we did not attempt to assess what a realistic global number might be.
It is even less clear how this net effect will change in response to global warming.
DK12 used ocean heat content (OHC) data for the upper 700 meters of oceans to draw three main conclusions: 1) that the rate of OHC increase has slowed in recent years (the very short timeframe of 2002 to 2008), 2) that this is evidence for periods of «climate shifts», and 3) that the recent OHC data indicate that the net climate feedback is negative, which would mean that climate sensitivity (the total amount of global warming in response to a doubling of atmospheric CO2 levels, including feedbacks) is low.
I understand the concept of summer to winter variation being a global warming response but the net change should be negative — and its not!
Li, P., Peng, C., Wang, M., Li, W., Zhao, P., Wang, K., Yang, Y. and Zhu, Q. (2017) «Quantification of the response of global terrestrial net primary production to multifactor global change.»
«The global mean climate responses to different forcings may differ because of the character of the forcings themselves (such as their geographical or vertical distribution) and because different forcings induce different patterns of surface warming or cooling, thereby affecting the net top - of - atmosphere radiation imbalance, and thus the ocean heat uptake rate.»
It was written in response to last December's Paris climate summit, which agreed a plan for cutting emissions to net zero after mid-century, and an intent to peg global warming to 1.5 C.
Climate scientists would say in response that changes in ocean circulation can't sustain a net change in global temperature over such a long period (ENSO for example might raise or lower global temperature on a timescale of one or two years, but over decades there would be roughly zero net change).
Re 416 Bernd Herd — in climate science, for global climate change, specifically a global (average surface) temperature change in response to a global (typically average net tropopause - level after stratospheric adjustment) radiative forcing (or other heat source — although on Earth those tend not to be so big), where the radiative forcing may be in units of W / m ^ 2, so that equilibrium climate sensitivity is in K * m ^ 2 / W (it is often expressed as K / doubling CO2 as doubling CO2 has a certain amount of radiative forcing for given conditions).
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