E&ES 359
Climate Change TTR
10:30-11:50AM ESC 405 Johan C. Varekamp
Climate change is common to this earth – we have known
ice ages and hyper thermals, snowball earth and who knows what is in store for
us for the rest of this century. We will study the way in which the climate
machine works, some effort will be made to study paleo climate indicators, and
we will put a large effort in studying the current period of global climate
change that may be human-activity driven. The role of CO2 in earth
processes is very large relative to the modest quantities of it that are
present in the atmosphere. We will therefore study many aspects of the physics,
chemistry and biology of CO2 and carry out several projects that
relate to CO2. In addition, we will look into the role of methane as
a modifier of climate and catastrophic methane releases as a feedback to
incipient warming. Several questions regarding CO2 will be
addressed:
- Is CO2
cycling the Òthermostat of the earthÓ?
- What
is the role of CO2 in global climate (greenhouse gas)?
- How
does photosynthesis works?
- How
does CO2 acidify surface waters and promote weathering?
- How
much CO2 is there on other planets?
- How
has atmospheric CO2 varied over the course of earth history?
- What
should we do to prevent further global warming - the Kyoto treaty
The course is a mixture of lectures, with handouts and a
bookchapters (Greenhouse Puzzles, by Wally Broecker) and student-run
experiments that deal with climate and the Carbon cycle on earth. We will also
sidestep to the link between art and climate, ranging from the color choices
that landscape painters make to provide a climate sense to the historical
painting record that portrays the changes in climate through dress, landscape
and skies. We will visit the studio of a landscape painter in NYC. There is a
midterm exam on the lectures (50%) and project reports that transition into
term papers and class presentations at the end (50%). The class participants
need initiative and a certain self-reliance to make it a rewarding and successful
experience.
There probably will be ~ 25-30 students in the class, with
5-6 projects over 2/3 of the semester. The projects have sign-up sheets and
ultimately 5 students per group will be selected by me after reading the
preferences and qualifications. The projects are:
- AEM
- Analog Earth Model – a model,
designed and built at the Wesleyan University workshop, of the earth
inside a water cooled box (=the universe). Visible light illuminates the Ôblack sphere earthÕ,
which radiates IRR that is then carried off by the water-cooled walls of
the cell. The box can be filled with Ar (radiatively neutral gas), CO2
(greenhouse gas) or mixtures thereof, and temperature sensors will
register the effect of adding the greenhouse gas. Experiments and
calculations are carried out by the AEM group to simulate the terrestrial
greenhouse effect in this analog matter. Requirements: capability
to collaborate, good quantitative skills, interest in Physics (radiation)
and love of fiddling with instruments (and patience). This is a totally
novel and never tried experiment!!
- GGA
- Greenhouse gas absorption of IRR
– The group builds an IRR absorption spectrometer from bits and
pieces already acquired on ebay. The goal is to measure the
wavelength-integrated absorption of IRR by CO2 through
measurements with different CO2 concentrations and different
pathlengths. These measurements can then be used to estimate the Ôblocking
powerÕ of CO2 gas in the natural atmosphere through
extrapolation to natural conditions. Requirements: capability to
collaborate, good quantitative skills, interest in Physics (radiation) and
love of fiddling with instruments (and patience). This is a novel
experiment!!
- MAC
- Middletown Air CO2
– The concentration of CO2 in the atmosphere increases as
a result of anthropogenic CO2 releases as well as natural
processes. What is the magnitude of CO2 concentration
variations in the Wesleyan University outside air over a semester? We
drilled a hole through a windowsill at the 4th floor of the ESC
and set up an instrument that samples the air and analyzes it for CO2
every 0.5 hour for most of the semester. This project is interrupted every
time the CO2 analyzer is needed for the other projects, so the
record consists of a time series with ÔholesÕ in it. Data storage,
plotting and treatment is an important part and models will be created to
explain the observed patterns. The MAC group may ask the local firestation
to use their ladder wagon to create a detailed atmospheric CO2
profile along the highest ladder during two time periods in a day. Requirements: interest in analysis of gases, data plotting,
creative thinking.
- CIW
– CO2 into Water
– Atmospheric CO2 dissolves into water through gas
exchange reactions. The increases in atmospheric CO2 are
partially buffered by the uptake of CO2 in surface waters,
mainly the oceans. The kinetics of CO2 uptake in fresh water
and seawater can be experimentally determined in a gas dissolution cell,
which we have already built. The CIW group will carry out experiments in
freshwater and in seawater, through gas dissolution in static water and in
stirred water (4 experiments in total). The obtained data will be plotted
and modeled, and compared with experimental results from others as well as
experiments in nature (e.g., rate of loss of atmospheric bomb 14C
to the oceans). Requirements: Interest in physical chemistry and
detailed experimentation, and scaling of models.
- CIP
–CO2 into Plants – Plants absorb atmospheric CO2 through photosynthesis,
and it is well known that the rate of photosynthesis increases with raised
atmospheric CO2 levels.
The CIP group will carry out plant growth experiments in
growthchambers under different temperature, CO2 and humidity
conditions (chambers courtesy to Dana Royer). Models will be used to scale
the results up to the terrestrial biosphere and atmosphere. Requirements:
Interest in plant physiology and biology, experimentation and model
scaling.
- CMCC
- Computer Models of Climate Change – The response of climate on changes in greenhouse gas
concentrations can be modelled through box modeling and computer climate
simulations. This can be extended by incorporating the ÔhumanÕ component
and entering human consumption patterns and choices into the box models.
Simple programs already exist and will be re-written for zero dimensional
climate models to simulate the various CO2-options, with
ground-truthing of the model on data of the last 100 years. Results may be
compared with externally acquired climate simulations. Requirements:
Interest in computer modeling, ability to generalize from very detailed
data sets to useful expresions, some insight in economics
- CTPST
– Carbon Trading Policies and Sequestration Technologies
Cutbacks in anthropogenic CO2
emissions can be made through technological advances in the western world
(e.g., CO2 sequestration) as well as exchange of technology with
lesser developed nations. ÔCarbon tradingÕ is another approach to limit net CO2
fluxes into the atmosphere (e.g., planting trees in Costa Rica).
The class has a small budget to acquire necessary items but
most are already available. The group spirit should be high and everyone should
pitch in – no slackers dumping work on others! Experiments are done in
room ESC 413 (back of Hg lab) and the class meets in ESC 405. When successful,
outreach efforts to local schools and colleges are encouraged.
Syllabus
January
24 Venus
is hot, Mars is cold, and what about Earth? Papers
29 The
modern earth climate: principles of radiative equilibrium - handouts
31 The
greenhouse effect – principles – handouts
February
5 More
greenhouse discussions
7 First Experiments meetings (I am out of town)
12 CO2
and long term climate change - the thermostat of the earth – papers
14 Chemical
Indicators of climate change - Stable Isotopes - papers
19 Chemical
Indicators of climate change - Radiogenic isotopes - papers
21 Climate
and Art
26 Second Experiments meeting (I am out of town)
28 Climate
and Art
March
4 The
short C cycle
6 Carbonate
chemistry in the oceans
25 Biological
processes, photosynthesis
27 14C
as a tool in climate studies
April
1 Other
carbon forms and their cycles (methane, CO)
3 Volcanoes
and climate
8 Historical
changes in climate – little ice age, medieval warm period
10 Modern
and historic anthropogenic carbon releases
15 Reducing
the anthropogenic carbon releases – Kyoto treaty - Bali
17 Climate
change and society – Mitigation or adaptation?
22 CO2
disposal and atmospheric clean-up
24 Future
climate: models, potential effects
29 Project presentations 1+2
May
1 Project presentations 3+4
6 Project presentations 5+6