On the future zonal contrasts of equatorial Pacific climate: Perspectives from Observations, Simulations, and Theories
Abstract Changes in the zonal gradients of sea surface temperature (SST) across the
equatorial Pacific have major consequences for global climate. Therefore, accurate future …
equatorial Pacific have major consequences for global climate. Therefore, accurate future …
Quantifying uncertainties in global and regional temperature change using an ensemble of observational estimates: The HadCRUT4 data set
CP Morice, JJ Kennedy, NA Rayner… - Journal of Geophysical …, 2012 - Wiley Online Library
Recent developments in observational near‐surface air temperature and sea‐surface
temperature analyses are combined to produce HadCRUT4, a new data set of global and …
temperature analyses are combined to produce HadCRUT4, a new data set of global and …
An ensemble data set of sea surface temperature change from 1850: The Met Office Hadley Centre HadSST. 4.0. 0.0 data set
JJ Kennedy, NA Rayner, CP Atkinson… - Journal of Geophysical …, 2019 - Wiley Online Library
One of the largest sources of uncertainty in estimates of global temperature change is that
associated with the correction of systematic errors in sea surface temperature (SST) …
associated with the correction of systematic errors in sea surface temperature (SST) …
Daily high-resolution-blended analyses for sea surface temperature
RW Reynolds, TM Smith, C Liu, DB Chelton… - Journal of …, 2007 - journals.ametsoc.org
Two new high-resolution sea surface temperature (SST) analysis products have been
developed using optimum interpolation (OI). The analyses have a spatial grid resolution of …
developed using optimum interpolation (OI). The analyses have a spatial grid resolution of …
Improvements to NOAA's historical merged land–ocean surface temperature analysis (1880–2006)
TM Smith, RW Reynolds, TC Peterson… - Journal of …, 2008 - journals.ametsoc.org
Observations of sea surface and land–near-surface merged temperature anomalies are
used to monitor climate variations and to evaluate climate simulations; therefore, it is …
used to monitor climate variations and to evaluate climate simulations; therefore, it is …
Reassessing biases and other uncertainties in sea surface temperature observations measured in situ since 1850: 2. Biases and homogenization
JJ Kennedy, NA Rayner, RO Smith… - Journal of …, 2011 - Wiley Online Library
Changes in instrumentation and data availability have caused time‐varying biases in
estimates of global and regional average sea surface temperature. The size of the biases …
estimates of global and regional average sea surface temperature. The size of the biases …
[HTML][HTML] Improved analyses of changes and uncertainties in sea surface temperature measured in situ since the mid-nineteenth century: The HadSST2 dataset
NA Rayner, P Brohan, DE Parker… - Journal of …, 2006 - journals.ametsoc.org
Improved Analyses of Changes and Uncertainties in Sea Surface Temperature Measured In
Situ since the Mid-Nineteenth Century: The HadSST2 Dataset in: Journal of Climate Volume …
Situ since the Mid-Nineteenth Century: The HadSST2 Dataset in: Journal of Climate Volume …
Historical estimates of surface marine temperatures
EC Kent, JJ Kennedy - Annual Review of Marine Science, 2021 - annualreviews.org
Surface temperature documents our changing climate, and the marine record represents
one of the longest widely distributed, observation-based estimates. Measurements of near …
one of the longest widely distributed, observation-based estimates. Measurements of near …
[HTML][HTML] In situ SST quality monitor (iQuam)
F Xu, A Ignatov - Journal of Atmospheric and Oceanic …, 2014 - journals.ametsoc.org
Brisson, A., Le Borgne P., and Marsouin A., 2002: Results of one year of preoperational
production of sea surface temperatures from GOES-8. J. Atmos. Oceanic Technol., 19, 1638 …
production of sea surface temperatures from GOES-8. J. Atmos. Oceanic Technol., 19, 1638 …
A large discontinuity in the mid-twentieth century in observed global-mean surface temperature
Data sets used to monitor the Earth's climate indicate that the surface of the Earth warmed
from∼ 1910 to 1940, cooled slightly from∼ 1940 to 1970, and then warmed markedly …
from∼ 1910 to 1940, cooled slightly from∼ 1940 to 1970, and then warmed markedly …