I've not tried to model faster - moving changes such as those related to ENSO, mainly because I'm not thus far persuaded that those have much bearing on
the mean global temperature for say the decade 2100 - 2110.
So, for example, HadCRU and GISS each provide a climatological datum of
mean global temperature for a single year and present it as a difference (i.e. an anomaly) from the average mean global temperature of a 30 year period.
The forecast for 2014 agrees with data from Jan - Oct, which shows
the mean global temperature for 2014 so far is 0.57 °C ** (+ / - 0.1 °C).
Re 440: «Could a model now predict
the mean global temperature for 2010 - 2015 accurately?
Not exact matches
Even the most optimistic estimates of the effects of contemporary fossil fuel use suggest that
mean global temperature will rise by a minimum of 2 °C before the end of this century and that CO2 emissions will affect climate
for tens of thousands of years.
Scientists working to improve storm intensity forecasting have identified a more accurate
means of predicting a hurricane's strength as it approaches landfall, using sea
temperature readings that they say will help forecasters better prepare communities
for storm impacts in the face of sea - level rise caused by rising
global temperatures.
And of course, exceeding the 1.5 °C threshold
for even an entire year would not
mean that
global temperatures had in fact risen to that point, never (at least within our lifetime) to drop back below it as it's too short of a timeframe to make that determination.
The Paris Agreement sets the goal of holding the increase in the
global average
mean temperature to well below 2 °C above preindustrial levels but calls
for efforts to limit that increase to 1.5 °C.
«We really can't detect these changes yet in the existing data in the way we can detect in changes,
for example, in the
global mean temperature,» he said.
The IPCC, in its most recent assessment report, lowered its near - term forecast
for the
global mean surface
temperature over the period 2016 to 2035 to just 0.3 to 0.7 degree C above the 1986 — 2005 level.
«The EU holds firmly to the commonly agreed objective of keeping the
global mean temperature increase below 2ºC,» the bloc's diplomats wrote, calling
for «urgent actions» to help countries meet their Copenhagen pledges and close that gap.
It explores a number of different climate change futures — from a no - emissions - cuts case in which
global mean temperatures rise by 4.5 °C, to a 2 °C rise, the upper limit
for temperature in the Paris Agreement.
If there was a 4.5 °C
global mean temperature rise, the climates in these areas are projected to become unsuitable
for many the plants and animals that currently live there
meaning:
Water changes
temperature more slowly than the air or land, which
means the
global ocean heat is likely to persist
for some time.
They then looked at what that
meant for the
temperature rise over the coming few decades, and found that
global warming this century will indeed be slower than thought.
«The first step was to reconstruct the history of
global mean temperatures for the last 784,000 years, using combined data from marine sediment cores, ice cores, and computer simulations covering the last eight glacial cycles,» said Friedrich, a post-doctoral researcher at IPRC.
The U.S. National Research Council (NRC) estimates that every degree Celsius of warming in
global average
temperatures means a 5 to 15 percent drop in yield, particularly
for corn, in North America.
He said he does think, however, that there will a broader shift to warmer ocean conditions that will last
for several years and that
means that
global temperatures will hover around the level they have recently reached before moving upward again, like stairs on a staircase.
Given that we're mainly looking at the
global mean surface
temperature anomaly, the most appropriate comparison is
for the net forcings
for each scenario.
Global mean temperatures averaged over land and ocean surfaces, from three different estimates, each of which has been independently adjusted
for various homogeneity issues, are consistent within uncertainty estimates over the period 1901 to 2005 and show similar rates of increase in recent decades.
The team increased one forcing agent (see sidebar) in a climate model,
for example carbon dioxide, and decreased another, say methane, so that
global mean temperature didn't change.
Using thus 10 different climate models and over 10,000 simulations
for the weather@home experiments alone, they find that breaking the previous record
for maximum
mean October
temperatures in Australia is at least six times more likely due to
global warming.
That
mean global tropospheric
temperature has
for the last 50 years fallen and risen in close accord with the SOI of 5 — 7 months earlier shows the potential of natural forcing mechanisms to account
for most of the
temperature variation.
«Solar cycle variability may therefore play a significant role in regional surface
temperatures, even though its influence on the
global mean surface
temperature is small (0.07 K
for December — February).»
Overall the results suggest that the Southern Oscillation exercises a consistently dominant influence on
mean global temperature, with a maximum effect in the tropics, except
for periods when equatorial volcanism causes ad hoc cooling.
Global mean temperature for the period January to September 2017 was 0.47 ° ± 0.08 °C warmer than the 1981 - 2010 average (estimated at 14.31 °C).
If the
temperature record does plainly show a level line of
global mean air
temperature for the period in question it apparently won't be «seen» by those who are dubious about my remarks.
Analyses of primate macroevolutionary dynamics provide support
for a diversification rate increase in the late Miocene, possibly in response to elevated
global mean temperatures, and are consistent with the fossil record.
Based on the linear trend,
for the 0 to 3,000 m layer
for the period 1961 to 2003 there has been an increase of ocean heat content of approximately 14.2 ± 2.4 × 1022 J, corresponding to a
global ocean volume
mean temperature increase of 0.037 °C during this period.
However, comparison of the
global, annual
mean time series of near - surface
temperature (approximately 0 to 5 m depth) from this analysis and the corresponding SST series based on a subset of the International Comprehensive Ocean - Atmosphere Data Set (ICOADS) database (approximately 134 million SST observations; Smith and Reynolds, 2003 and additional data) shows a high correlation (r = 0.96)
for the period 1955 to 2005.
For example, the
global -
mean near - surface air
temperature was more than 1 K lower than in the experiment assuming spherical snow grains.
Five hundred to seven hundred million years ago, our planet had what scientists have determined to be another severe period of cold, with the
global mean temperature somewhere around 10 degrees F. Again, hardly a good candidate planet
for life.
He then uses what information is available to quantify (in Watts per square meter) what radiative terms drive that
temperature change (
for the LGM this is primarily increased surface albedo from more ice / snow cover, and also changes in greenhouse gases... the former is treated as a forcing, not a feedback; also, the orbital variations which technically drive the process are rather small in the
global mean).
ECS is defined in terms of
global mean temperature change, not separately
for land and ocean.
Moreover,
for temperatures similar to the present
global mean, water vapor feedback actually cancels out some of the positive curvature from the fourth - power law (see Chapter 4 of my book, Principles of Planetary Climate).
[9]
Temperature changes Global mean surface temperature difference from the average for 1880 &m
Temperature changes
Global mean surface
temperature difference from the average for 1880 &m
temperature difference from the average
for 1880 — 2009.
Going back further, that
temperature was about 1.8 °F (1 °C) above the average
for the second half of the 19th century,
meaning global temperatures are already halfway to 2 °C (4 °F) above preindustrial levels.
Here's the problem forests and forest managers face under climate change: Increasing
global mean temperatures, changes in precipitation, and the hydrologic cycle are expected to lead to
temperature and drought stress
for many tree species.
For three particular mismatches — sea ice loss rates being much too low in CMIP3, tropical MSU - TMT rising too fast in CMIP5, or the ensemble
mean global mean temperatures diverging from HadCRUT4 — it is likely that there are multiple sources of these mismatches across all three categories described above.
If
mean global temperatures trending significantly upward over the last 100 years isn't worrying enough
for you, how about that giant piece of Antarctica that is about to crack off and sink into the ocean... I don't know how the existence of
global warming is still a debate!
If as suggested here, a dynamically driven climate shift has occurred, the duration of similar shifts during the 20th century suggests the new
global mean temperature trend may persist
for several decades.
/ / Corrections
for the discontinuity are expected to alter the character of mid-twentieth century
temperature variability but not estimates of the century - long trend in
global -
mean temperatures.
Now, when we know the the
global mean temperature for 2016, it's even more obvious.
«Our results show that
temperature records of at least 17 years in length are required
for identifying human effects on
global -
mean tropospheric
temperature.»
The adjustments are unlikely to significantly affect estimates of century - long trends in
global -
mean temperatures, as the data before, 1940 and after the mid-1960s are not expected to require further corrections
for changes from uninsulated bucket to engine room intake measurements.
Human - caused CO2 emissions are the main reason, among others,
for the rapidly rising
global mean temperatures our NASA scientists are documenting with more accuracy that ever before due to technological advances and scope of the research.
The surface
temperature increase that partially gave rise to concerns about
global warming coincided with a move to tethered electronic measuring devices (um, I think that
means thermometers) that forced the movement of many stations closer to buildings and developed areas, causing warming that may not have been corrected
for.
For example, a rise in
global mean temperature will almost certainly lead to an increase in the incidence of record high
temperatures.
Note that if we were only looking at the
global mean temperature, there would be quite a lot of wiggle room
for different contributions.
Joe cites to a very recent article that re-estimates
global mean temperature in two ways that might offset some of the bias
for under - sampling the arctic in one existing
global data set.