T - 5: S. Wofsy (Harvard) HIAPER Pole to Pole Observations (HIPPO) of climatically important gases and aerosols 10:35 - 10:55 T - 6: R. Muller (UC Berkeley) The Berkeley
Earth Surface Temperature Land Results 10:55 - 11:15 T - 7: R. Rohde (Berkeley Temp Project) A new estimate of the Earth land surface temperature 11:15 - 11:35 T - 8: F. Singer (SEPP) Is the reported global surface warming of 1979 to 1997 real?
Not exact matches
The Tibetan Plateau in China experiences the strongest monsoon system on
Earth, with powerful winds — and accompanying intense rains in the summer months — caused by a complex system of global air circulation patterns and differences in
surface temperatures between
land and oceans.
The equator promises relatively happy
landings on relatively smooth
surfaces, but it also guarantees
temperatures that exceed 250 degrees Fahrenheit during the day and plummet below — 240 °F during the night — and both day and night last 14
Earth days.
The researchers looked at annual maximum
land surface temperatures averaged across 8 - day periods throughout the year for every 1 - square kilometer (247 acres) pixel on
Earth.
It was the discovery of a consistent year - to - year profile that allowed the researchers to move beyond a previous analysis, in which they identified the hottest spots on
Earth, to the development of a new global - change indicator that uses the entire planet's maximum
land surface temperatures.
According to his Berkeley
Earth Surface Temperature project, the average temperature on land has risen 1.5 degrees Celsius — roughly 2.7 degrees Fahrenheit —
Temperature project, the average
temperature on land has risen 1.5 degrees Celsius — roughly 2.7 degrees Fahrenheit —
temperature on
land has risen 1.5 degrees Celsius — roughly 2.7 degrees Fahrenheit — since 1753.
For their paper, published in Applied Geography, researchers at the
Earth Institute at Columbia University and Battelle Memorial Institute studied air
temperature data from weather stations,
land surface temperatures measured by satellites and socioeconomic data.
Pierre, could you comment on what, exactly, is new in the recent Philipona paper, compared with the two similar papers they published last year («Greenhouse forcing outweighs decreasing solar radiation driving rapid
temperature rise over
land», «Radiative forcing — measured at
Earth's
surface — corroborate the increasing greenhouse effect»)?
Again, Monckton must surely know full well that for the last 25 - 30 years satellite
temperature measurement of sea and
land surface have replaced terrestrial
temperature station measurements in many cases since these give a much greater coverage (70 % of the
surface of the
Earth is water... it's difficult to put weather stations on top of ice sheets etc.!)
Most of
Earth's
land surfaces were warmer than average or much warmer than average, according to the Land & Ocean Temperature Percentiles map above, with record warmth notable across most of equatorial and northeastern South America and parts of southeastern A
land surfaces were warmer than average or much warmer than average, according to the
Land & Ocean Temperature Percentiles map above, with record warmth notable across most of equatorial and northeastern South America and parts of southeastern A
Land & Ocean
Temperature Percentiles map above, with record warmth notable across most of equatorial and northeastern South America and parts of southeastern Asia.
On the whole, the
Earth's
land surface has «greened» in response to rising CO2 emissions and warmer
temperatures, but these new results suggest there could also be a negative impact of climate change on vegetation growth in North America.
Berkeley
Earth was created to address potential biases in the
land surface temperature record.
Ray, I think Lee Grable's point is important: The fact that we use the term «global
temperature» to mean the average
temperature on a two - dimensional
surface rather than the three - dimensional ocean plus
land plus atmosphere system of the
earth has the potential to allow confusion.
The two longest ones are of
temperature near the
Earth's
surface: a vast network of weather stations over
land areas, and ship data from the oceans.
After all, if average
surface temperature is 15 C, wouldn't you expect
land and ocean below the
surface to equilibrate at roughly that
temperature (with a slightly rising gradient to account for the flow of
Earth's internal heat)?
For those not familiar with it, the purpose of Berkeley
Earth was to create a new, independent compilation and assessment of global
land surface temperature trends using new statistical methods and a wider range of source data.
The new paper, «A New Estimate of the Average
Earth Surface Land Temperature Spanning 1753 to 2011,» has been posted, along with extensive related material, including a list of responses to frequent questions, including these:
My amateur spreadsheet tracking and projecting the monthly NASA GISS values suggests that while 2018 and 2019 are likely to be cooler than 2017, they may also be the last years on
Earth with global average
land and ocean
surface temperature anomaly below 1C above pre-industrial average (using 1850 - 1900 proxy).
Global average
temperature is lower during glacial periods for two primary reasons: 1) there was only about 190 ppm CO2 in the atmosphere, and other major greenhouse gases (CH4 and N2O) were also lower 2) the
earth surface was more reflective, due to the presence of lots of ice and snow on
land, and lots more sea ice than today (that is, the albedo was higher).
But even when carbon dioxide does make its way out of the atmosphere,
Earth's natural systems can release other carbon dioxide molecules that were previously stored in the oceans /
land back into the atmosphere, making the full effect of carbon dioxide emissions on
surface temperatures much longer than this 5 - 200 year average.
As far as I am aware,
temperatures of the atmosphere close to the
surface, rather than the actual
surface, are usually measured over
land, unless measured remotely by satellites, in which case the
temperature of the material overlaying the
Earth's
surface is measured, rarely the
surface itself.
I also think that if one wishes to prove that carbon dioxide in the atmosphere is the cause of global warming then the focus of
temperature measurement should be upon those few feet between the
Earth's
surface and the measuring instruments employed on
land for measuring that
temperature.
See Rohde et al., A New Estimate of the Average
Earth Surface Land Temperature Spanning 1753 to 2011, Geoinformatics & Geostatistics 2013.
(To learn more about
land surface temperatures and air
temperatures, read: Where is the Hottest Place on
Earth?)
WebHubTelescope @ # 25 Also there's Prof. Richard Muller's
land surface only AST since 1753 from 36,000
temperature stations at Berkeley
Earth.
They publish
land and sea +
land temperatures, it should be posible to extract the sea part given that we know it is 70 % of the total
Earth surface.
«A New Estimate of the Average
Earth Surface Land Temperature Spanning 1753 to 2011.»
Berkeley
Earth video representation of the
land surface temperature anomaly, 1800 to the present.
Earth Atmospheric
Land Surface Temperature and Station Quality in the Contiguous United States
Water takes longer to heat up and cool down than does the air or
land, so ocean warming is considered to be a better indicator of global warming than measurements of global atmospheric
temperatures at the
Earth's
surface.
To get a complete picture of
Earth's
temperature, scientists combine measurements from the air above
land and the ocean
surface collected by ships, buoys and sometimes satellites, too.
Other GMST series based on
land temperature stations and sea
surface temperatures from ships and buoys are now available and are regularly updated, such as those from the Japanese Meteorological Agency and Berkeley
Earth.
Almost all
land surfaces on
Earth experienced unusually warm
temperatures in February 2016.
As others have noted, the IPCC Team has gone absolutely feral about Salby's research and the most recent paper by Dr Roy Spencer, at the University of Alabama (On the Misdiagnosis of
Surface Temperature Feedbacks from Variations in
Earth's Radiant Energy Balance), for one simple reason: both are based on empirical, undoctored satellite observations, which, depending on the measure required, now extend into the past by up to 32 years, i.e. long enough to begin evaluating real climate trends; whereas much of the Team's science in AR4 (2007) is based on primitive climate models generated from primitive and potentially unreliable
land measurements and proxies, which have been «filtered» to achieve certain artificial realities (There are other more scathing descriptions of this process I won't use).
Working like a thermometer in the sky, the sensor measures thermal infrared radiation to take the
temperature of
Earth's
land surfaces.
Land surface temperatures reflect how hot the
surface of the
Earth would feel to the touch in a particular location.
This analysis is in the paper «
Earth Atmospheric
Land Surface Temperature and Station Quality in the United States», available here.
Earth Surface: (A)
Land - based air
temperature observation.
Berkeley
Earth was founded in early 2010 with the goal of addressing the major concerns of skeptics regarding global warming and the
land surface temperature record.
Life on
land, argues Schwartzman, has intensified the chemical weathering of rocks such that carbon dioxide has been removed from the atmosphere and the
surface temperature of the
Earth has remained cooler than if life had not been present - a kind of inverted global warming.
Rohde, R. et al: «A new estimate of the average
earth surface land temperature spanning 1753 to 2011», Manuscript: text presented at the 3rd Santa Fe conference on global and regional climate
temperature change, 2011
The original Escalator was based on the Berkeley
Earth Surface Temperature (BEST) data, which incorporates more temperature station data than any other data set, but is limited to land - only data; additionally the record terminates in
Temperature (BEST) data, which incorporates more
temperature station data than any other data set, but is limited to land - only data; additionally the record terminates in
temperature station data than any other data set, but is limited to
land - only data; additionally the record terminates in early 2010.
The three major groups calculating the average
surface temperature of the
earth (
land and ocean combined) all are currently indicating that 2014 will likely nudge out 2010 (by a couple hundredths of a degree Celsius) to become the warmest year in each dataset (which begin in mid-to-late 1800s).
This created a qualitative transformation in Homo sapiens» impact on
earth system trends: levels of carbon dioxide, nitrous oxide, methane, stratospheric ozone,
surface ocean
temperature, ocean acidification, marine fish capture, coastal nitrogen, tropical forest depletion,
land domestication and terrestrial biosphere degradation.
One result of the Berkeley
Earth kriging approach is the construction of a
temperature field for the entire
land surface, such that every location on the
land has an estimated
temperature that is a function of latitude, longitude, altitude, climatology, and a residual — or weather.
However, these sites do not provide even or comprehensive coverage of the
Earth's
surface, nor are the sites immune to contamination from
land - use changes — all of which add noise and uncertainty to the world
temperature measurements.
Estimates of
temperature variations near the
earth's
surface are based on thermometer readings taken daily at thousands of
land stations and on board thousands of ships.
Third, the distribution of
land and water on the
Earth's
surface; which controls its
temperature distribution, moisture availability, monsoon effects, hurricanes, and other storm tracks.
Last month the Berkeley
Earth Surface Temperature Project released the findings of its extensive study on global
land temperatures over the past century.
Figure 2: Berkeley
Earth Surface Temperature (BEST) land - only surface temperature data (green) with linear trends applied to the timeframes 1973 to 1980, 1980 to 1988, 1988 to 1995, 1995 to 2001, 1998 to 2005, 2002 to 2010 (blue), and 1973 to 2010
Surface Temperature (BEST) land - only surface temperature data (green) with linear trends applied to the timeframes 1973 to 1980, 1980 to 1988, 1988 to 1995, 1995 to 2001, 1998 to 2005, 2002 to 2010 (blue), and 1973 to
Temperature (BEST)
land - only
surface temperature data (green) with linear trends applied to the timeframes 1973 to 1980, 1980 to 1988, 1988 to 1995, 1995 to 2001, 1998 to 2005, 2002 to 2010 (blue), and 1973 to 2010
surface temperature data (green) with linear trends applied to the timeframes 1973 to 1980, 1980 to 1988, 1988 to 1995, 1995 to 2001, 1998 to 2005, 2002 to 2010 (blue), and 1973 to
temperature data (green) with linear trends applied to the timeframes 1973 to 1980, 1980 to 1988, 1988 to 1995, 1995 to 2001, 1998 to 2005, 2002 to 2010 (blue), and 1973 to 2010 (red).