[Response: The effect on the data actually used by Steig et al for the results featured in the paper (the satellite - derived ice
surface temperature estimates) is precisely zero.
Hence, the data sparseness during the early period of record is the major source of underlying uncertainty in
the surface temperature estimates.
Rind, D., and D. Peteet, 1985: Terrestrial conditions at the last glacial maximum and CLIMAP sea -
surface temperature estimates: Are they consistent?
You mean they weren't talking about the differences between satellite and
surface temperature estimates?
Assuming a full - glacial temperature lapse rate of -6 °C / 1000m, depression of mean annual temperature in glaciated alpine areas was ca 5.4 ± 0.8 °C; it is similar to values of temperature depression (5 - 6.4 °C) for the last glaciation obtained from various terrestrial sites, but contrasts with tropical sea -
surface temperature estimates that are only 1 - 3 °C cooler than present.
We can compare that to what results from subtracting the average of
surface temperature estimates from the average of satellite measurements:
The problem with under - coverage of polar and remote regions for representation on global
surface temperature estimates even so late as today is a shameful comment on how little commitment to understanding our world better those with resources have.
Many researchers seem to have assumed that the weather station - based estimates are much more reliable and consistent than the Sea
Surface Temperature estimates.
However, the CRU global mean combined land air / sea
surface temperature estimates for Jan - Aug 2005 lag behind the 1998 annual mean estimate by 0.08 C (0.50 C vs. 58C for 1998) while GISS indicates a lag of 0.02 C.
(a — c)
Surface temperature estimate for the past 65.5 Myr, including an expanded time scale for (b) the Pliocene and Pleistocene and (c) the past 800000 years.
Not exact matches
Schmidt's rough
estimate, which he posted on Twitter, is based on the extraordinary and unprecedented warming over the past 12 months, during which time global
surface temperatures have shot past the 1 °C above pre-industrial level.
Their data showed that the difference between polar and equatorial sea
surface temperatures in the Eocene was an
estimated 20 degrees Celsius, about 36 degrees Fahrenheit.
In addition to
temperature and precipitation, VIC's groundwater recharge
estimates take into consideration a particular location's land
surface, vegetation and soil type.
Current methods can
estimate the size and
temperature of an exoplanet planet in order to determine whether liquid water could exist on the planet's
surface, believed to be one of the criteria for a planet hosting the right conditions for life.
Kepler 22b: Most Earth - like This world, announced last December, is twice the diameter of our planet, and its
estimated surface temperature is a balmy 90 degrees Fahrenheit.
By measuring the remaining difference — the 20,000 - year old ice deep in the West Antarctic ice sheet is about 1 degree Celsius cooler than the
surface — the scientists were able to
estimate the original
temperature based on how fast pure ice warms up.
The government dataset, called the National Oceanic and Atmospheric Administration's Extended Reconstructed Sea
Surface Temperature version 4, increased the sea surface temperature trend estimate over the last 18 years from 0.07 ° Celsius per decade to 0.12 ° Celsius per decade, partly because of adjustments for different types of measuring instr
Surface Temperature version 4, increased the sea surface temperature trend estimate over the last 18 years from 0.07 ° Celsius per decade to 0.12 ° Celsius per decade, partly because of adjustments for different types of measuring i
Temperature version 4, increased the sea
surface temperature trend estimate over the last 18 years from 0.07 ° Celsius per decade to 0.12 ° Celsius per decade, partly because of adjustments for different types of measuring instr
surface temperature trend estimate over the last 18 years from 0.07 ° Celsius per decade to 0.12 ° Celsius per decade, partly because of adjustments for different types of measuring i
temperature trend
estimate over the last 18 years from 0.07 ° Celsius per decade to 0.12 ° Celsius per decade, partly because of adjustments for different types of measuring instruments.
Estimated increase in methane emissions if boreal lake
surface temperatures rise 1 degree Celsius
To
estimate the
temperature at various depths (from 3,500 m to 9,500 m depth) the researchers have used the heat flow and
temperatures at 1,000 m and 2,000 m provided in the Atlas of Geothermal Resources in Europe, as well as thermal data of the land
surface available from NASA.
Using infrared in near darkness through very little atmosphere, the team received data enabling it for the first time to
estimate the
surface temperatures over the planet's night side.
Executive Summary The Berkeley Earth
Surface Temperature project was created to make the best possible estimate of global temperature change using as complete a record of measurements as possible and by applying novel methods for the estimation and elimination of systema
Temperature project was created to make the best possible
estimate of global
temperature change using as complete a record of measurements as possible and by applying novel methods for the estimation and elimination of systema
temperature change using as complete a record of measurements as possible and by applying novel methods for the estimation and elimination of systematic biases.
The project, called
Estimating the Circulation and Climate of the Ocean (ECCO), uses observational data — including ocean
surface topography,
surface wind stress,
temperature, salinity profiles and velocity data — collected between June 2005 and December 2007.
Hurricanes are powered by energy pulled out of warm seawater, so sea
surface temperature data collected by satellites is fed into forecast models to
estimate their intensity.
They
estimated that land - use changes in the continental United States since the 1960s have resulted in a rise in the mean
surface temperature of 0.25 degree Fahrenheit, a figure Kalnay says «is at least twice as high as previous
estimates based on urbanization alone.»
Global
surface temperatures in 2016 averaged 14.8 degrees Celsius (58.64 °F), or 1.3 C (2.3 F) higher than
estimated before the Industrial Revolution ushered in wide use of fossil fuels, the EU body said.
The
surface temperature during reentry is
estimated up to 1750 °C for 15 minutes.
The planet is extremely close to its star — its orbital radius is only about three times the radius of the star — and the scientists have
estimated that its
surface temperatures may be as high as 3,000 degrees Kelvin, or more than 5,000 degrees Fahrenheit.
Starting in the late 1990s, scientists began using sophisticated methods to combine proxy evidence from many different locations in an effort to
estimate surface temperature changes during the last few hundred to few thousand years.
Using methods that allow them to
estimate the average stellar illumination and
temperatures on their
surfaces, scientists have already identified dozens of locations where life could potentially exist.
An ad hoc committee was formed, with the group carefully composed to include the breadth and depth of expertise and perspectives needed to analyze all aspects of how
surface temperatures are
estimated and interpreted and to comment generally on climate science.
One could assume that there was minimal global mean
surface temperature change between 1750 and 1850, as some datasets suggest, and compare the 1850 - 2000
temperature change with the full 1750 - 2000 forcing
estimate, as in my paper and Otto et al..
(Bottom) Patterns of linear global
temperature trends from 1979 to 2005
estimated at the
surface (left), and for the troposphere (right) from the
surface to about 10 km altitude, from satellite records.
That study addressed a puzzle, namely that recent studies using the observed changes in Earth's
surface temperature suggested climate sensitivity is likely towards the lower end of the
estimated range.
The range (due to different data sets) of global
surface warming since 1979 is 0.16 °C to 0.18 °C per decade compared to 0.12 °C to 0.19 °C per decade for MSU
estimates of tropospheric
temperatures.
Thus, not unlike tree rings, data on corals also can be calibrated to
estimate (sea)
surface temperatures (Beckman and Mahoney, 1998).
Global mean
surface temperatures have risen by 0.74 °C ± 0.18 °C when
estimated by a linear trend over the last 100 years (1906 — 2005).
[Response: The study quoted uses the difference between the weather models and the mostly independent
surface temperature record to
estimate a residual trend.
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.
Firstly, what is the best
estimate of the global mean
surface air
temperature anomaly?
We argue that KELT - 18b's high
temperature and low
surface gravity, which yield an
estimated ~ 600 km atmospheric scale height, combined with its hot, bright host make it an excellent candidate for observations aimed at atmospheric characterization.
When the CLIMAP data proved to be wrong, and was replaced by more reliable
estimates showing a substantial tropical
surface temperature drop, Lindzen had to abandon his then - current model and move on to other forms of mischief (first the «cumulus drying» negative water vapor feedback mechanism, since abandoned, and now the «Iris» effect cloud feedback mechanism).
This involves a combination of satellite observations (when different satellites captured
temperatures in both morning and evening), the use of climate models to
estimate how
temperatures change in the atmosphere over the course of the day, and using reanalysis data that incorporates readings from
surface observations, weather balloons and other instruments.
Since the mid 1970's, global
estimates of the potential destructiveness of hurricanes show an upward trend strongly correlated with increasing tropical sea -
surface temperature.
However, they were able to
estimate the
surface temperature of the companion star and found that it is about 2,000 degrees Celsius hotter than the
surface of the Sun.
Here we use basin - scale climate indices and regional
surface temperatures to
estimate loggerhead sea turtle (Caretta caretta) nesting at a variety of spatial and temporal scales.
At the planet's orbital distance of only 0.014 AU from its host star, however, the
surface temperature has been
estimated to be around 400 ° Fahrenheit (200 ° Celsius), which is way too hot for liquid water.
Whether the observed solar cycle in
surface temperature is as large as.17 K (as in Camp and Tung) or more like.1 K (many previous
estimates) is somewhat more in doubt, as is their interpretation in terms of low thermal inertia and high climate sensitivity in energy balance models.
Gregory et al. (2002) used observed interior - ocean
temperature changes,
surface temperature changes measured since 1860, and
estimates of anthropogenic and natural radiative forcing of the climate system to
estimate its climate sensitivity.
The series of reports concludes: «The recent pause in global
surface temperature rise does not invalidate previous
estimates of climate sensitivity.
the low ECS
estimates they obtain when using data from AMIP simulations (those where models are driven by observed evolving sea -
surface temperature patterns as well evolving forcing) are not news.