Not exact matches
Temperature changes relative to the corresponding
average for 1901 - 1950 (°C) from decade to decade from 1906 to 2005 over the Earth's continents, as well as the entire globe, global land area and the global ocean (lower graphs).
* Surface
temperature changes relative to 20th Century global
average (1901 - 2000) Source data NOAA - NCEI State of the Climate: Global Analysis [Web + data download]
Our result would peg the
average land
temperature change during the 1810s as about -0.7 C (+ / - 0.4 C at 95 %)
relative to the 19th century
average, which is broadly consistent with prior estimates.
The efficacy of a forcing is the climate sensitivity (in terms of global
average surface
temperature change per unit global
average RF) of that forcing
relative to a standard type of forcing.
[Response I'm not sure what point you are trying to make here, but if you feel that you can only assess whether
temperatures are
changing by looking at 30 - year
averages, consider the following: Global mean
temperature anomalies (in degrees C,
relative to 1961 - 90 reference period): 1885 - 1914: -0.35; 1915 - 1944: -0.18; 1945 - 1974: -0.07; 1975 - 2004: +0.21.
Relatively (it's always
relative changes that are most relevant to breaking the climate
averages) cool waters from the Caribbean have over recent weeks and months increasingly spread to the northeast, across the Atlantic Gulf Stream, creating a negative
temperature anomaly around the islands of the Azores and reaching further to the British Isles and the North Sea, where sea water is low due to the very cold December.
The program calculates trends in
temperature anomalies — not absolute
temperatures — but
changes relative to the
average temperature for the same month during the period of 1951 - 1980.
Model projections for precipitation
changes are less certain than those for
temperature.12, 2 Under a higher emissions scenario (A2), global climate models (GCMs) project
average winter and spring precipitation by late this century (2071 - 2099) to increase 10 % to 20 %
relative to 1971 - 2000, while
changes in summer and fall are not expected to be larger than natural variations.
Maps show projected
change in
average surface air
temperature in the later part of this century (2071 - 2099)
relative to the later part of the last century (1970 - 1999) under a scenario that assumes substantial reductions in heat trapping gases (B1) and a higher emissions scenario that assumes continued increases in global emissions (A2).
GISS measures the
change in global surface
temperatures relative to
average temperatures from 1951 to 1980.
The old story line: People need to worry about climate
change because doubling the atmosphere's concentration of carbon dioxide
relative to its preindustrial level would probably raise global
average temperatures by 2.7 to 8 degrees Fahrenheit.
The percentage «remaining» in the atmosphere seems to correlate well with the annual
change in global
average temperature compared to the previous year, with years of
relative warming showing higher % - age of the emitted CO2 «remaining» in the atmosphere.
Rather than dealing with trends, instead we ask how much has the TLT satellite brightness
temperature vertically
relative weighted
average changed in absolute levels, compared to what we'd find year to year or within groups of years.
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.
22 Land areas are projected to warm more than the oceans with the greatest warming at high latitudes Annual mean
temperature change, 2071 to 2100
relative to 1990: Global
Average in 2085 = 3.1 o C
The analyses are based on calculating
temperature differences at one point in time
relative to the
average over a certain period (anomalies) and creating a time series of
averaged global
temperature change.
The
temperature changes are
relative to the global
average surface
temperature of 1961 - 1990.
The map below presents the estimated
change in
average surface air
temperature for 2014
relative to the thirty - year
average from 1981 to 2010.
Projections for global
average temperatures relative to 1850 - 79 (upper chart), rates of glacier
change (middle) and total glacier mass (lower chart) for the 21st century.
«Based on all above findings and our compilation (Figure 4.4, Table 4.1 ″) we estimate that on
average 20 % to 30 % of species assessed are likely to be at increasingly high risk of extinction from climate
change impacts possibly within this century as global mean
temperatures exceed 2 °C to 3 °C
relative to pre-industrial levels (this chapter).
This paper assesses the three pathways in the light of Working Group I's recently released contribution to the Intergovernmental Panel on Climate
Change Fifth Assessment Report (IPCC 2013), which provided three specific global carbon dioxide (CO2) budgets, and associated them with specific risks of a global surface
temperature increase of more than 2 °C by the end of this century,
relative to the 1850 — 1900
average.
Probability density functions from different studies for global mean
temperature change for the SRES scenarios B1, A1B and A2 and for the decades 2020 to 2029 and 2090 to 2099
relative to the 1980 to 1999
average (Wigley and Raper, 2001; Knutti et al., 2002; Furrer et al., 2007; Harris et al., 2006; Stott et al., 2006b).