Title: How to study
1How to study
- Course and lecture goals!
2Efficiency
- A 100g bar of chocolate contains about 500 kcal
2100 kJ of chemical energy. If ones body can
convert it to 315kJ of mechanical energy we say
that the efficiency is 315/2100 15 - Similarly if a car engine converts 20 of
chemical energy contained in gas to mechanical
energy we say that its efficiency is 20.
3- Combining these two equations
- s TEarth4 e s TA4 s Ts4
- TA4 Ts4 /2
- we have s TEarth4 e s Ts4/2 s Ts4
- Ts4 2TEarth4/(2-e)
- Analyzing the infrared absorption
- curve gives average e 0.9
- so we obtain
- Ts 23 ºC
4Earth Energy Balance
- The more complex models involving multilayer
atmosphere partly transparent in infrared are
coming up with proper average temperature of the
surface of the Earth, which is about 15 ºC - The process we followed is the process of
consecutive approximation in modeling. Very often
we start with a very simple model and progress to
more complicated once getting (hopefully) closer
and closer to reality.
5Different layers of the atmosphere
6Earth Energy Balance
7Feedback Negative feedback and its role in
keeping the equilibrium
- Examples
- thermostat,
- steering wheel corrections on a straight road,
- water level in the toilet reservoir.
- Bull and Bear markets negative feedback
- Bull market a prolonged period in which
investment prices (shares) rise - bear market a prolonged period in which
investment prices fall
8Feedback Positive feedback and its role in
leading to catastrophe
- Examples
- reverse connected steering wheel,
- water level in the toilet reservoir with badly
connected valve. - Bull and Bear markets positive feedback
9Greenhouse Effect
- http//phet.colorado.edu/web-pages/simulations-bas
e.html
10History of Earth Climate
http//vathena.arc.nasa.gov/curric/land/global/cli
mchng.html
11History of Earth Climate
http//vathena.arc.nasa.gov/curric/land/global/cli
mchng.html
12History of Earth Climate How do we know it?
- The geological record of carved mountain valleys,
scratched bedrock, and glacial debris and
moraines gives evidence of the past several
million years. - Recently, cores have been removed from the ice at
Vostok Station in Antarctica. The longest cores
are about 2000 meters, sampling layers of ice
deposited as early as 160,000 years ago. The ice
trapped bubbles of air when it froze. The ratio
of oxygen isotopes in this air indicates the
average air temperature at the time the bubble
was trapped in ice. The bubbles also trap
atmospheric greenhouse gases that can be
measured. - Fossil plants and the distribution of pollen show
that vegetation has changed, consistent with
changing climate. Pollen from plants, buried in
shallow deposits of earth, indicate the
distribution of vegetation since the last
glaciation, about 20,000 years ago. Ancient
Plant Distribution describes how vegetation has
changed as the ice retreated, and offers a
student activity. - Tree rings provide a record of the weather back
3,000 years in some cases, and hundreds of years
in many areas. See Tree Rings, a Study of Climate
Change. - The historical record speaks to us for some 2,000
years and there have been real quantitative
measurements since about 1850.
http//vathena.arc.nasa.gov/curric/land/global/cli
mchng.html
13Feedback in the Earth's climate system
- Albedo effects positive feedback
- Snowball Earth
- Black Earth
- Final state how the feedback mechanism ends?
- Ways out
- Volcano eruptions,
- Large asteroid impact
14What may influence climate
- Solar activity
- Earth orbit
- Earth axis tilt
- Volcanoes
- nuclear winter or ash winter
- deposits
- Asteroid impacts
15History of the climate
- Climate and human history
- Journey webpage
- Why worry now?
16Solar movie
17(No Transcript)
18Greenhouse Effect
- http//phet.colorado.edu/web-pages/simulations-bas
e.html
19Absorption in the infrared region.
20Positive Feedback example in climate
- CO2 is a greenhouse gas.
- It dissolves in water.
- As the temperature increases the solubility of
CO2 decreases. - Increase of amount of CO2 leads to increase of
temperature, which leads to release of CO2 from
the oceans. - Positive feedback.
- Notice that a small increase of CO2 in the
atmosphere can start this process
21Negative Feedback example in climate
- Increase in temperature increases evaporation
rate of water from the Oceans and therefore
increases the amount of cloud cover. The
increased cloud thickness or extent increases
Earths Albedo and therefore could reduce
incoming solar radiation and limit warming. - On the other hand it is not obvious that if
additional cloud cover happens at what latitudes
and at what times might it occur. Also it is not
obvious what types of clouds might be generated.
Thick low clouds would have a stronger ability to
block sunlight than extensive high (cirrus) type
clouds.
http//www.globalchange.umich.edu/globalchange1/cu
rrent/lectures/samson/feedback_mechanisms/
22The same process can create both positive and
negative feedback
- Increase of the amount of water vapor in the
atmosphere increases the cloud cover and so
decreases the temperature. - But the water is a greenhouse gas so the increase
in temperature would permit more water vapor to
be stored in the atmosphere. The amount of water
vapor the atmosphere can hold increases
exponentially with temperature so increases in
temperature can yield increases in atmospheric
water vapor. The increased water vapor, as a
greenhouse gas, enhances the greenhouse effect
and could lead to further warming as long as this
positive feedback isn't modified by an increase
in cloud cover that could lead to a negative
feedback.
http//www.globalchange.umich.edu/globalchange1/cu
rrent/lectures/samson/feedback_mechanisms/
23Compelling evidence for global warming
- Temperature curves
- Glaciers and arctic ice disappearing
- Possible explanations
- Continuation of warming after little ice age in
middle ages - Solar activity
- Human influence
- Modeling of the climate.
- Difficulties
- Model testing
- Fits, available amount of data (remember fitting
to 4 points and than to more during the lab?)
24http//vathena.arc.nasa.gov/curric/land/global/cli
mchng.html
The last century curve
25Temperature variation last 150 years
26(No Transcript)
27If humans, than what we did?
- Greenhouse gases
- Ozone layer
- What is the influence of ozone layer on climate
- Ozone layer destructive gases
- Deforestation - what is the feedback effect here?
28The net effect of Ozone depletion on Earth
temperature is cooling. It is a greenhouse gas in
the region different from CO2 and H2O
http//www.ipcc.ch/press/SPM.pdf
29http//www.globalchange.umich.edu/globalchange1/cu
rrent/lectures/samson/feedback_mechanisms/
30Sophisticated climate models
31We will discuss the effects of energy production
later
32August 4, 2007Walking to the shops damages
planet more than going by car
- Food production as a source of greenhouse gases.
- Assumptions made by the author of this statement
- The caloric intake needed to walk taken solely
from beef. - No accounting of making and recycling of the car
33Other controversial statements about the climate
changes
- Traditional nappies are as bad as disposables, a
study by the Environment Agency found. While
throwaway nappies make up 0.1 per cent of
landfill waste, the cloth variety are a waste of
energy, clean water and detergent - Paper bags cause more global warming than
plastic. They need much more space to store so
require extra energy to transport them from
manufacturers to shops - Diesel trains in rural Britain are more polluting
than 4x4 vehicles. Douglas Alexander, when
Transport Secretary, said If ten or fewer
people travel in a Sprinter train, it would be
less environmentally damaging to give them each a
Land Rover Freelander and tell them to drive - Burning wood for fuel is better for the
environment than recycling it, the Department for
Environment, Food and Rural Affairs discovered - Organic dairy cows are worse for the climate.
They produce less milk so their methane emissions
per liter are higher - Someone who installs a green light bulb undoes
a years worth of energy-saving by buying two
bags of imported vegetables, as so much carbon is
wasted flying the food to Britain - Trees, regarded as shields against global warming
because they absorb carbon, were found by German
scientists to be major producers of methane, a
much more harmful greenhouse gas - Sources Defra How to Live a Low-Carbon Life, by
Chris Goodall Absorbent Hygiene Products
Manufacturers Association The Times BBC
34- Prof. John Mitchell OBE FRS, Chief Scientist at
the Met Office explores some of the common myths
about climate change.The Met Office recognises
that climate change is a complex subject. There
are genuine areas of uncertainty and scientific
controversy. There are also a number of
misunderstandings and myths which are recycled,
often by non-climate scientists, and portrayed as
scientific fact.Recent coverage has questioned
the influence of humans on the climate. While the
arguments used might have been regarded as
genuine areas of sceptical enquiry 20 years ago,
further observed warming and advances in climate
science render these out of touch. Myth 1 - Ice
core records show that changes in temperature
drive changes in carbon dioxide, and it is not
carbon dioxide that is driving the current
warming - Levels of atmospheric CO2 are higher than at any
time in the last 430,000 years Click on the image
for a larger view Only the first part of this
statement is true. Over the several hundred
thousand years covered by the ice core record,
the temperature changes were primarily driven by
changes in the Earths orbit around the sun. Over
this period, changes in temperature did drive
changes in carbon dioxide (CO2). Concentrations
of CO2 are now much higher and increasing much
faster than at any time in at least the last
600,000 years. This should be a warning that what
is happening now is very different to what
happened in the past. In fact, over the last 100
years CO2 concentrations have increased by 30
due mainly to human-induced emissions from fossil
fuels. Because CO2 is a greenhouse gas, the
increased concentrations have contributed to the
recent warming and probably most of the warming
over the last 50 years.The bottom line is that
temperature and CO2 concentrations are linked. In
recent ice ages, natural changes in the climate
(due to orbit changes for example) led to cooling
of the climate system. This caused a fall in CO2
concentrations which weakened the greenhouse
effect and amplified the cooling. Now the link
between temperature and CO2 is working in the
opposite direction. Human-induced increases in
CO2 is enhancing the greenhouse effect and
amplifying the recent warming. Myth 2 - Solar
activity is the main driver of climate change - Temperature change, 1850-2000 Click on the image
for a larger viewThere are many factors which may
contribute to climate change. For example, over
the last million years most of the long-term
changes in climate were probably due to small but
well understood changes in the Earths orbit
around the Sun. Over much of the last 1,000 years
most of the variability can probably be explained
by cooling due to major volcanic eruptions and
changes in solar heating.However, the situation
in the 20th century is more complicated. There is
some evidence that increases in solar heating may
have led to some warming early in the 20th
century, but direct satellite measurements show
no appreciable change in solar heating over the
last three decades. Three major volcanic
eruptions in 1963, 1982 and 1991 have led to
short periods of cooling. Throughout the century
CO2 increased steadily and has been shown to be
responsible for most of the warming in the second
half of the century. The final piece of the
jigsaw is that as well as producing CO2, burning
fossil fuels also produces small particles called
aerosols which cool the climate by reflecting
sunlight back into space. These have increased
steadily in concentration over the 20th century,
which has probably offset some of the warming we
have seen. Only when all of these factors are
included do we get a satisfactory explanation of
the magnitude and patterns of climate change over
the last century.The bottom line is that changes
in solar activity do affect global temperatures.
However, what research also shows is that
increased greenhouse gas concentrations have a
much greater effect than changes in the Suns
energy over the last 50 years. Myth 3 - There is
less warming in the upper atmosphere than at the
surface which disproves human-induced warming - We expect greater warming in the upper atmosphere
than at the surface in the tropics, but the
reverse is true at high latitudes. This
expectation holds whether the cause of warming is
due to greenhouse gases or changes in the Suns
output. Until recently, measurements of the
temperature changes in the tropics in recent
decades did not appear to show greater warming
aloft than at the surface. It has now been shown
that allowing for uncertainties in the
observations, the theoretical and modelling
results can be reconciled with the
observations.The bottom line is that the range of
available information is now consistent with
increased warming through the troposphere (the
lowest region of the atmosphere). Myth 4 - The
intensity of cosmic rays changes climate - Solar activity, 1850-2000 Click on the image for
a larger viewA recent experiment has apparently
shown that gamma radiation can form ions
(electrically charged particles) in the
atmosphere. Under certain circumstances, these
can subsequently form ultra-fine particles (or
aerosols), which could conceivably act as cloud
condensation nuclei (CCN) and therefore form
clouds. However, the mechanism by which cosmic
rays might affect climate is as yet purely
speculative and unquantified. While it has long
been known that radiation could form ions and, in
theory, ultimately lead to cloud formation, the
importance of this process compared to all the
other major sources of particles and CCN has not
been proven. Indeed, there is no evidence that
the flux of cosmic rays has decreased over the
last 30 years.The bottom line is, even if cosmic
rays have a detectable effect on climate (and
this remains unproven), measured solar activity
over the last few decades has not significantly
changed and cannot explain the continued warming
trend. In contrast, increases in CO2 are well
measured and its warming effect is well
quantified. It offers the most plausible
explanation of most of the recent warming and
future increases. Myth 5 - Climate models are too
complex and uncertain to provide useful
projections of climate change - There have been major advances in the development
and use of models over the last 20 years. The
models are based mainly on the laws of physics.
There are also empirical techniques which use,
for example, studies of detailed processes
involved in cloud formation. The most advanced
computer models also include detailed coupling of
the circulations of atmosphere and oceans, along
with detailed descriptions of the feedbacks
between all components of the climate system
including the cryosphere and biosphere. Climate
models have been used to reproduce the main
features of the current climate, the temperature
changes over the last hundred years and the main
features of the Holocene (6,000 years ago) and
Last Glacial Maximum (21,000) years ago.The
bottom line is that current models enable us to
attribute the causes of past climate change and
predict the main features of the future climate
with a high degree of confidence. We now need to
provide more regional detail and more complete
analysis of extreme events. Met Office work on
climate change - The Met Office Hadley Centre was opened in the
early 1990s and is a world-leading climate
centre. It has over 150 world-renowned climate
experts who draw from the expertise of the
supercomputer modellers at the Met Office.It is
the UKs official centre for climate change
research partly funded by Defra (the Department
for Environment Food and Rural Affairs) and MOD
which provides in-depth information and advice to
the Government on climate change issues.It
undertakes studies of the global climate using
similar, though more extensive, models of the
atmosphere used for the prediction of weather
conditions.It informs the work of the
Intergovernmental Panel on Climate Change (IPCC)
and was the leading UK contributor to the Fourth
Assessment Review published in February 2007. It
assembled much of the scientific basis of the
Stern Review on the Economics of Climate Change
(pub. October 2006). Its research also informs
the UK Climate Impacts Programme on how climate
change will impact at regional and national
levels in the UK.It advises businesses and
governments on the science of climate change and
strategies for mitigation and adaptation.Media
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