CO 2, 14 C, the Sun and Climate Change over the Last Millennium 1. CO 2 and climate variability (Gerber et al.,2003) 2. 14 C and solar activity (Muscheler.
NATS 101 Lecture 33 Climate Change (cont’d). Absorption 20% of incident Visible (0.4-0.7 m) is absorbed O 2 an O 3 absorb UV (shorter than 0.3 m)
Numerical modelling of possible catastrophic climate changes E.V. Volodin, N. A. Diansky, V.Ya. Galin, V.P. Dymnikov, V.N. Lykossov Institute of Numerical.
NATS 101 Lecture 25 Climate Change (cont’d)
Detecting human influence on extreme daily temperature at regional scales
The O rbiting C arbon O bservatory ( OCO ) Mission
CO 2 , 14 C, the Sun and Climate Change over the Last Millennium
OUTLINE Examples of AMOC variability and its potential predictability, Why we care,
Projected distributions of novel and disappering climates by 2100 AD
Dynamical Simulations in North Atlantic Tropical Cyclone Activity using Observed Low-Frequency SST Oscillation Imposed on CMIP5 Model RCP4.5 SST Projections
COUPLED ATMOSPHERE-OCEAN GSM (INMCM3.0)
Global Warming
