COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE

Ph. D. physics, Author, Speaker at self employed
Jan. 13, 2015
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE
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COUNTER-INTUITY OF COMPLEX SYSTEMS: WEATHER VS. CLIMATE

Editor's Notes

  1. The temperature increase curve coincides with the temperature increase.
  2. Oceanic heat sink. Evolution of the ocean heat content (OHC) at several depths of the global ocean between 1980 and 2011. Since 2000, the subsurface ocean has warmed much faster than in the preceding two decades; this ocean warming may explain why average atmospheric temperatures have not risen during the past decade. The gray bars show the timing of the El Chichón and Pinatubo volcanic eruptions. The yellow and blue bars show the timing of several key El Niño and La Niña events. Data from the ORAS-4 ocean reanalysis (10).
  3. Integrated OHC.Integrated from the surface to different indicated depths in the global ocean (A), the Atlantic (B), the Pacific (C), the Southern Ocean (D), and the Indian Ocean (E). Shown is the 12-month running mean deviation from the climatological mean (1970 to 2012) for each layer, so attention should not be focused on the absolute distance between the curves but should be on their relative changes in time. Color lines show the OHC in the left scale, in units of 1023 J. The black line shows the mean SST up to 2013. (Insets) The division of the globe into the Pacific, the Atlantic, the Indian Ocean, and the Southern Ocean. Although shown in the figure, data in the earlier decades were not as reliable (see Data and Materials and Methods); the discussion in the text is focused on the better-observed regions and periods.