Sentences with phrase «sea surface temperature variability from»

Castro S. L., W. J. Emery, G. A. Wick and W. Tandy (October 2017): Submesoscale Sea Surface Temperature Variability from UAV and Satellite Measurements.

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.

Not exact matches

«Winds hide Atlantic variability from Europe's winters: Study reveals how wind patterns change along with sea - surface temperatures.»

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).

Further investigation of the variability of Arctic surface temperature and sea ice cover was performed by analyzing data from a coupled ocean — atmosphere model.

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.

Offshore, mean monthly sea surface temperatures range from 15.4 °C to 20.1 °C [3], but in the nearshore upwelling region, variability is greater and temperatures range from 10 °C to 18 °C [4].

Reconstructing twentieth - century sea surface temperature variability in the southwest Pacific: A replication study using multiple coral Sr / Ca records from New Caledonia.

''... 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.»

Forced variability results from boundary conditions, such as sea - surface temperatures, and natural or internal variability results from the chaotic nature of dynamical systems1, 2.