That illustrates my point, which is that
present changes in surface temperature is not a good indicator of what we should expect in the future, and as such, it is not a great idea to make the debate about the observed ocean temperature.
Not exact matches
The climate
change «hockey stick» is a graph first published
in 1998 by Michael Mann et al. that attempted to reconstruct the mean
surface temperature on the planet during the period A. D. 900 to the
present, using multiple proxies, such as tree rings, to measure
temperatures before formal instrumentation was
in use.
We
present a new modeling system that predicts both internal variability and externally forced
changes and hence forecasts
surface temperature with substantially improved skill throughout a decade, both globally and
in many regions.
The substantial uncertainties currently
present in the quantitative assessment of large - scale
surface temperature changes prior to about A.D. 1600 lower our confidence
in this conclusion compared to the high level of confidence we place
in the Little Ice Age cooling and 20th century warming.»
Your earlier # 182 was equally disconcerting where you quoted Norris and Slingo (2009) saying «At
present, it is not known whether
changes in cloudiness will exacerbate, mitigate, or have little effect on the increasing global
surface temperature caused by anthropogenic greenhouse radiative forcing.»
A conceptual model is
presented where, through a number of synergistic processes and positive feedbacks,
changes in the ultraviolet / blue flux alter the dimethyl sulphide flux to the atmosphere, and
in turn the number of cloud condensation nuclei, cloud albedo, and thus sea
surface temperature.
Consequently, as they say slightly earlier
in the abstract: «At
present, it is not known whether
changes in cloudiness will exacerbate, mitigate, or have little effect on the increasing global
surface temperature caused by anthropogenic greenhouse radiative forcing.»
Present estimates are that limiting the increase
in global average
surface temperature to no more than 2 — 2.5 °C above its 1750 value of approximately 15 °C will be required to avoid the most catastrophic, but certainly not all, consequences of climate
change.
Here we show that accounting for recent cooling
in the eastern equatorial Pacific reconciles climate simulations and observations.We
present a novel method of uncovering mechanisms for global
temperature change by prescribing,
in addition to radiative forcing, the observed history of sea
surface temperature over the central to eastern tropical Pacific
in a climate model.
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.
Yes, if the sentence is taken to refer to statistically significant
change in surface temperature up to
present.
We
present an analysis to illustrate why
temperature values at specific levels will depend on wind speed, and with the same boundary layer heat content
change, trends
in temperature should be expected to be different at every height near the
surface when the winds are light, as well as different between light wind and stronger wind nights.
The idea is, if the
change in surface temperature over that period is affected by
changes in cloud cover, but
changes of the
surface temperature associated with the ocean warming are small, then
changes in cloud cover must be driving the
present global warming.
If there is deep - water formation
in the final steady state as
in the
present day, the ocean will eventually warm up fairly uniformly by the amount of the global average
surface temperature change (Stouffer and Manabe, 2003), which would result
in about 0.5 m of thermal expansion per degree celsius of warming, calculated from observed climatology; the EMICs
in Figure 10.34 indicate 0.2 to 0.6 m °C — 1 for their final steady state (year 3000) relative to 2000.
The map below
presents the estimated
change in average
surface air
temperature for 2014 relative to the thirty - year average from 1981 to 2010.
No one knows when the
present plateau
in the mean
surface air
temperature will end nor whether the
change will be warmer or cooler.
«We
present a new modeling system that predicts both internal variability and externally forced
changes and hence forecasts
surface temperature with substantially improved skill throughout a decade, both globally and
in many regions.
The scatter diagrams described and
presented on these pages depict projected
changes in seasonal
surface air
temperature and precipitation for three 30 - year periods (2010 - 2039, 2040 - 2069 and 2070 - 2099) relative to the baseline period 1961 - 1990
in 32 sub-continental scale regions (see below).
We have two new entries to the long (and growing) list of papers appearing the
in recent scientific literature that argue that the earth's climate sensitivity — the ultimate rise
in the earth's average
surface temperature from a doubling of the atmospheric carbon dioxide content — is close to 2 °C, or near the low end of the range of possible values
presented by the U.N.'s Intergovernmental Panel on Climate
Change (IPCC).
Although historical records indicate that atmospheric CO2 concentrations and sea
surface temperatures have undergone significant oscillations and have exceeded
present - day levels
in the past [3,4], it is the unprecedented rates of
change that are fuelling concerns over whether organisms will retain the capacity to mediate vital ecosystem functions and services [5,6].
We
present a novel method of uncovering mechanisms for global
temperature change by prescribing,
in addition to radiative forcing, the observed history of sea
surface temperature over the central to eastern tropical Pacific
in a climate model.