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The Physics of the
Climate System “Warming of the climate system is unequivocal, and since the 1950s, many
of the observed changes are unprecedented over decades to millennia. The
atmosphere and ocean have warmed, the amounts of snow and ice have diminished,
sea level has risen, and the concentrations of greenhouse gases have
increased.” This statement in the Fifth Assessment
Report of the Intergovernmental Panel on Climate Change (IPCC) in 2013 is based
on a wide variety of climate observations and model simulations. The
present characteristics of the climate system are a product of a long-term
evolution determined by external forcing (sun, volcanoes) and internal
interactions within the climate system, which is composed of atmosphere, ocean,
cryosphere, land surfaces, and the marine and terrestrial biosphere. Until 250
years ago, the interference of man was small, and climate variations were a
product of natural processes and interactions alone. Since the beginning of industrialisation
the composition of the atmosphere, especially the concentrations of greenhouse
gases, such as carbon dioxide and methane, have significantly increased. In
addition, the character of the land surface has been largely modified through
land-use and land-cover change through human activities. Most of the observed
global warming during the past 100 years is attributed to these anthropogenic
impacts. This course provides the evidence of climate
variations on all time-scales and their response to human impacts, and presents
an introduction to the physics of the climate system, with a special focus on
atmosphere, ocean and ice. Exercises in the afternoons will deal with specific
climate processes and with the energy balance of the Earth and other planets. Special topics are: ·
evidence
for climate variations on a variety of time-scales from in-situ measurements,
remote sensing techniques, climate archives, and palaeo-climate proxies, ·
physical
properties of the climate system and its components (atmosphere, ocean, ice), ·
physical
processes relevant for climate variability and change, ·
simple
models of the climate system (energy balance models, Daisy World), ·
climate
scenarios from complex coupled climate models, ·
new
results from the latest IPCC reports.