The rainfall variability emerges out
of sea surface temperature variability in the Pacific Ocean.
Original study: Messié, M. and F.P. Chavez, 2011: Global modes
of sea surface temperature variability in relation to regional climate indices.
They found a 60 - to 90 - year cycle in Barents and Greenland seas ice extent related to the Atlantic Multidecadal Oscillation (AMO); the AMO is a basin - wide cycle
of sea surface temperature variability similar to the El Niño and La Niña cycles in the Pacific, but varying over much longer periods.
The component
of sea surface temperature variability that maximizes its integral time scale, obtained from the combination of 14 control runs of CMIP3 climate models.
Not exact matches
So this effect could either be the result
of natural
variability in Earth's climate, or yet another effect
of carbon dioxide and other greenhouse gases like water vapor trapping more heat and thus warming
sea -
surface temperatures.
But Haris Majeed, a Master's student in Medical Imaging at U
of T's Faculty
of Medicine, wondered if long - term climate
variability in
sea surface temperatures played a role.
The results suggest that the impact
of sea ice seems critical for the Arctic
surface temperature changes, but the
temperature trend elsewhere seems rather due mainly to changes in ocean
surface temperatures and atmospheric
variability.
The findings suggest the latitude
of the Atlantic jet stream in summer is influenced by several factors including
sea surface temperatures, solar
variability, and the extent
of Arctic
sea - ice, indicating a potential long - term memory and predictability in the climate system.
In recent years, a brand
of research called «climate attribution science» has sprouted from this question, examining the impact
of extreme events to determine how much — often in fractional terms — is related to human - induced climate change, and how much to natural
variability (whether in climate patterns such as the El Niño / La Niña - Southern Oscillation,
sea -
surface temperatures, changes in incoming solar radiation, or a host
of other possible factors).
El Niño is a weather pattern characterized by a periodic fluctuation in
sea surface temperature and air pressure in the Pacific Ocean, which causes climate
variability over the course
of years, sometimes even decades.
Checkley, D. M. Jr & Lindegren, M.
Sea surface temperature variability at the Scripps Institution
of Oceanography Pier.
Figure 4 - Spatial
variability of the
sea surface temperature (SST) trends scaled with the global
surface air
temperature (SAT) trend for each simulation used in the study.
Mestas - Nunez, A.M., and D.B. Enfield, 1999: Rotated global modes
of non-ENSO
sea surface temperature variability.
«Multidecadal
variability of Atlantic tropical cyclone activity is observed to relate to the Atlantic Multidecadal Oscillation (AMO)-- a mode manifesting primarily in
sea surface temperature (SST) in the high latitudes
of the North Atlantic.
Changes here have a long term effect, affecting the strength
of the north - ward horizontal flow
of the Atlantic's upper warm layer, thereby altering the oceanic poleward heat transport and the distribution
of sea surface temperature (SST — AMO), the presumed source
of the (climate) natural
variability.
Further investigation
of the
variability of Arctic
surface temperature and
sea ice cover was performed by analyzing data from a coupled ocean — atmosphere model.
Another region
of sea surface temperature (SST)
variability that impacts on Australian climate is located in the Indian Ocean.
DelSole et al 2011 provide a convenient figure (top
of post) summarizing the spatial structure
of low frequency
variability of sea surface temperature in an ensemble
of GCMs.
The evolution
of El Niño - Southern Oscillation (ENSO)
variability can be characterized by various ocean - atmosphere feedbacks, for example, the influence
of ENSO related
sea surface temperature (SST)
variability on the low - level wind and
surface heat fluxes in the equatorial tropical Pacific, which in turn affects the evolution
of the SST.
Rodríguez - Fonseca, B., E. Mohino, C.R. Mechoso, C. Caminade, M. Biasutti, M. Gaetani, J. Garcia - Serrano, E.K. Vizy, K. Cook, Y. Xue, I. Polo, T. Losada, L. Druyan, B. Fontaine, J. Bader, F.J. Doblas - Reyes, L. Goddard, S. Janicot, A. Arribas, W. Lau, A. Colman, M. Vellinga, D.P. Rowell, F. Kucharski, and A. Voldoire, 2015:
Variability and predictability
of West African droughts: A review
of the role
of sea surface temperature anomalies.
For example, let's say that evidence convinced me (in a way that I wasn't convinced previously) that all recent changes in land
surface temperatures and
sea surface temperatures and atmospheric
temperatures and deep
sea temperatures and
sea ice extent and
sea ice volume and
sea ice density and moisture content in the air and cloud coverage and rainfall and measures
of extreme weather were all directly tied to internal natural
variability, and that I can now see that as the result
of a statistical modeling
of the trends as associated with natural phenomena.
One dynamically downscaled IPCC simulation (WRF - MPI - ECHAM5) has a robust representation
of Pacific
sea surface temperature variability in the future projection period up to 2040, but the relationship to enhancement
of precipitation extremes is not as clear as in observations.
They are largest in regions
of high
sea surface temperature variability such as the western boundary currents and along the northern boundary
of the Southern Ocean.
They write in their abstract: «The Pacific decadal oscillation (PDO), defined as the leading empirical orthogonal function
of North Pacific
sea surface temperature anomalies, is a widely used index for decadal
variability.
''... worked with two sediment cores they extracted from the seabed
of the eastern Norwegian
Sea, developing a 1000 - year proxy
temperature record «based on measurements
of δ18O in Neogloboquadrina pachyderma, a planktonic foraminifer that calcifies at relatively shallow depths within the Atlantic waters
of the eastern Norwegian
Sea during late summer,» which they compared with the temporal histories
of various proxies
of concomitant solar activity... This work revealed, as the seven scientists describe it, that «the lowest isotope values (highest
temperatures)
of the last millennium are seen ~ 1100 - 1300 A.D., during the Medieval Climate Anomaly, and again after ~ 1950 A.D.» In between these two warm intervals,
of course, were the colder
temperatures of the Little Ice Age, when oscillatory thermal minima occurred at the times
of the Dalton, Maunder, Sporer and Wolf solar minima, such that the δ18O proxy record
of near -
surface water
temperature was found to be «robustly and near - synchronously correlated with various proxies
of solar
variability spanning the last millennium,» with decade - to century - scale
temperature variability of 1 to 2 °C magnitude.»
The research will be directed toward using a combined observational and modeling approach to investigate the nature and cause
of the Congo rainfall
variability in the 20st century, with an emphasis on the role
of global
sea surface temperatures.
Importantly, the changes in cereal yield projected for the 2020s and 2080s are driven by GHG - induced climate change and likely do not fully capture interannual precipitation
variability which can result in large yield reductions during dry periods, as the IPCC (Christensen et al., 2007) states: ``... there is less confidence in the ability
of the AOGCMs (atmosphere - ocean general circulation models) to generate interannual
variability in the SSTs (
sea surface temperatures)
of the type known to affect African rainfall, as evidenced by the fact that very few AOGCMs produce droughts comparable in magnitude to the Sahel droughts
of the 1970s and 1980s.»
Kandiano, E. S., Bauch, H. A. & Müller, A.
Sea surface temperature variability in the North Atlantic during the last two glacial - interglacial cycles: comparison
of faunal, oxygen isotopic, and Mg / Ca - derived records.
Decadal variations in the North Pacific Gyre Oscillation are characterized by a pattern
of sea surface temperature anomalies that resemble the central Pacific El Niño, a dominant mode
of interannual
variability with far - reaching effects on global climate patterns5, 6, 7.
«Causes
of differences in model and satellite tropospheric warming rates» «Comparing tropospheric warming in climate models and satellite data» «Robust comparison
of climate models with observations using blended land air and ocean
sea surface temperatures» «Coverage bias in the HadCRUT4
temperature series and its impact on recent
temperature trends» «Reconciling warming trends» «Natural
variability, radiative forcing and climate response in the recent hiatus reconciled» «Reconciling controversies about the «global warming hiatus»»
Tourre, Y. M., Y. Kushnir, and W. B. White, 1999: Evolution
of interdecadal
variability in
sea level pressure,
sea surface temperature, and upper ocean
temperature over the Pacific Ocean.
Numerous factors have been shown to influence these local
sea surface temperatures, including natural
variability, human - induced emissions
of heat - trapping gases, and particulate pollution.
Over these shorter periods, there are many modes
of climate
variability, usually involving semi-structured oscillations in
sea surface temperatures, like the El Niño - Southern Oscillation, the Pacific Decadal Oscillation, the Arctic Oscillation, and so on.
The simulated
sea surface temperature variability from two global coupled climate models for the second half
of the 20th century is dominated by natural internal
variability associated with the Antarctic Oscillation, suggesting that the models» internal
variability is too strong, leading to a response to anthropogenic forcing that is too weak.
Our results have important implications concerning the influence
of North Atlantic
sea surface temperatures on East Asian climate, and provide support for the possibility
of an AMO signature on global multidecadal climate
variability.»
Published in the Journal
of Climate, authors Richard Seager and Martin Hoerling cleverly used climate models forced by
sea surface temperatures to separate how much
of the past century's North American droughts have been caused by ocean
temperatures, natural
variability, and humans.
Regional circulation patterns have significantly changed in recent years.2 For example, changes in the Arctic Oscillation can not be explained by natural variation and it has been suggested that they are broadly consistent with the expected influence
of human - induced climate change.3 The signature
of global warming has also been identified in recent changes in the Pacific Decadal Oscillation, a pattern
of variability in
sea surface temperatures in the northern Pacific Ocean.4
In a new paper, researchers conclude that changes in sensible heat transfer and evaporation fluxes — in response to strong regional trends in the air -
surface temperature contrast related to the changing character
of the
sea ice cover — are becoming increasingly consequential to Arctic climate
variability and change.
Other researchers are investigating
variability in the Pacific Ocean, including a measure
of sea surface temperatures known as the Pacific Decadal Oscillation (PDO).
Jacox M. G., M. A. Alexander, C. A. Stock and G. Hervieux (March 2017): On the skill
of seasonal
sea surface temperature forecasts in the California Current System and its connection to ENSO
variability.
Additionally, such an observing system, by measuring the temporal and spatial
variability of the AMOC for approximately a decade, would provide essential ground truth to AMOC model estimates and would also yield insight into whether AMOC changes or other atmospheric / oceanic
variability have the dominant impact on interannual
sea surface temperature (SST)
variability.
The PDO does not represent the multidecadal
variability in the
sea surface temperatures of the North Pacific.
Thus, in numerical weather prediction out to a mere few days, one tends to neglect the intrinsic
variability of the oceans and concentrates on the atmosphere, with
sea surface temperatures prescribed as a boundary condition; the
sea surface temperature field can either be kept constant in time or allowed to vary in some prescribed manner, e.g., according to a diurnal cycle.
Natural
Variability Doesn't Account for Observed
Temperature Increase In it's press release announcement, NASA points out that while there are other factors than greenhouse gases contributing to the amount of warming observed — changes in the sun's irradiance, oscillations of sea surface temperatures in the tropics, changes in aerosol levels in the atmosphere — these factors are not sufficient to account for the temperature increases observed
Temperature Increase In it's press release announcement, NASA points out that while there are other factors than greenhouse gases contributing to the amount
of warming observed — changes in the sun's irradiance, oscillations
of sea surface temperatures in the tropics, changes in aerosol levels in the atmosphere — these factors are not sufficient to account for the
temperature increases observed
temperature increases observed since 1880.
Note that this result is not directly a test
of model fidelity, but rather
of linearity; what is converging here is the model's representations
of air -
sea interaction leading to global mean
surface temperature anomalies, not whether the models have the ability to capture the magnitude or even the spatial patterns
of observed RASST
variability.
Title:
Variability of sea -
surface temperature and
sea - ice cover in the Fram Strait over the last two millennia Author (s): Bonnet, S; de Vernal, A; Hillaire - Marcel, C, et al..
This model, when forced with observed
sea surface temperatures and atmospheric conditions, can reproduce the observed rise in hurricane counts between 1980 and 2012, along with much
of the interannual
variability (Figure 5).
For future projections, GFDL atmospheric modelers have developed global models capable
of simulating many aspects
of the seasonal and year - to - year
variability of tropical cyclone frequency in a number
of basins, using only historical
sea surface temperatures as input.
Alexander M. A., J. D. Scott, K. D. Friedland, K. E. Mills, J. A. Nye, A. J. Pershing and A. C. Thomas (January 2018): Projected
sea surface temperatures over the 21st century: Changes in the mean,
variability and extremes for large marine ecosystem regions
of Northern Oceans.
Feb 8: Projected
sea surface temperatures over the 21st century: Changes in the mean,
variability and extremes for Large Marine Ecosystem regions
of Northern Oceans