Carbon Footprint
Carbon Footprint. Carbon Footprint Exercise
1) Go to https://www.carbonfootprint.com/calculator.aspx
2) Calculate your carbon footprint. For each tab (Welcome, House, Flights, etc.) fill in the information asked for.
Save your time - order a paper!
Get your paper written from scratch within the tight deadline. Our service is a reliable solution to all your troubles. Place an order on any task and we will take care of it. You won’t have to worry about the quality and deadlines
Order Paper Now3) If it doesn’t apply to you, skip that tab.
4) If you live in a dorm and your academic institution does not provide the information, you can use information from your parent’s bills and calculate your footprint making the assumption you still live there.
5) When you are done entering all your information, go to the results page. Take a screenshot of the results and paste it into your Word or pdf document.
6) Answer the following questions.
a) What is a carbon footprint?
b) What makes the greatest contribution to your CO2 emissions?
c) What are carbon offsets?
d) The goal of this assignment was for you to learn about all the potential contributions to the carbon cycle you are part of. What were your major take-home lessons from this exercise? If you are interested in making changes, what would they be? What types of changes do you think would require societal change (infrastructure, technology) before you could make a significant change?
12/13/17
1
What Determines Global Temperatures?
What determines the radiative budget of the planet?
• Solar radiation from sun • Lost radiation back to space
• Absorbed radiation retained by planet
Radiative Forcings A radiative forcing is a factor that changes the
balance between radiation coming into the atmosphere and radiation going out.
Radiative Forcings Radiative forcing is a factor that changed in
the balance between radiation coming into the atmosphere and radiation going out.
Positive forcings tend on average to warm the
surface of the earth
Radiative Forcings Radiative forcing is a factor that changed in
the balance between radiation coming into the atmosphere and radiation going out.
Positive forcings tend on average to warm the
surface of the earth
Negative forcings tend on average to cool the surface of the earth.
12/13/17
2
Radiative forcings & feedbacks* •  Positive
– Greenhouse gases – Tropospheric ozone – Solar radiation – Black carbon on snow (also aerosols) – Water vapor* – Albedo* – loss of sea ice and snow cover.
•  Negative – Aerosols (clouds* and industrial aerosols) – Albedo – Landuse
Radiative forcings can change independent of global
temperatures
Feedbacks are “forcings” that change with temperature.
Greenhouse gases
How do we know increases in these gases increase global
temperatures?
Historical Correlation
Quantum Mechanics
O2 and N2 do not absorb and emit energy from photons with
wavelengths in the infrared range.
Greenhouse gases do and in all
directions.
Weather versus Climate?
12
12/13/17
3
Weather vs. Climate • Weather
– Time scale: minutes to seasons – Spatial scale: local to regional
• Climate – Time scale: averaged of years and decades – Spatial scale: regional to global – Patterns of weather over long periods
• Hurricanes • Droughts • Precipitation • etc.
13
Global Temperatures
How do we measure the earth’s temperature?
15
Instrumental Record Thermometers and Satellites
16 1840’s to present 1978 to present
Instrumental Record • Weather stations around the world • Data collected by several different
research groups. – NASA Goddard Institute of Space Studies
(GISS) – National Oceanographic and Atmospheric
Administration (NOAA) national Climate data Center (NCDC)
– Hadley Centre of the UK Meteorological Office (HADCRUT)
• They quality check the data and produce analyzed data sets. 17
Berkeley Earth Surface Temperature study (BEST) • Richard Muller – physicist who was
skeptical of other groups work • Analyzed global data using a different
methodology and additional data •  Found same patterns as other groups
18
12/13/17
4
Satellites • Measure temperature indirectly by
irradiance and at different layers of atmosphere
• Two groups analyze data • Remote Sensing Systems (RSS) • University of Alabama, Huntsville (UAH) • Both groups show warming trend
– RSS, 0.162 oC per decade – UAH, 0.138 oC per decade – Instrumental 0.2 oC per decade 19
Proxy Record
20
Temperature Proxies • Proxy
– something that reliably changes with temperature.
– Needs to be comparable to present measurements. Something that changed both before and and after the instrumental record.
• Types of Proxies – Isotopes in organisms and rocks – Isotopes in ice cores – Stratigraphic profiles of organisms – Tree ring data
21
During the ice ages, how did global temperatures fluctuate?
23
Pattern during ice ages • Changes from 4 oC to 7 oC • Change since last ice age of about 4 oC • Abrupt changes in Ice ages occur over
5000 to 10,000 years • Last 150 years 0.99 oC and predictions for
200 year period between 2 oC to 6 oC. • Causes of changes different
24
12/13/17
5
Since the last ice age, how do global temperatures fluctuate?
The last 1,800 years
The last 1,000 years 1,800 year global pattern
• Warmer today than anytime in that period • Medieval Climate Anomaly (800 – 1200 AD) • Little Ice Age (1550 – 1850 AD)
28
Pattern since industrial revolution
29 base period 1951-1980
12/13/17
6
Why is the Arctic warming so fast?
31
Arctic Warming
Arctic Warming 2 times global rate
Arctic Amplification • Sea ice acts as a reflector which cools the
Arctic. • As Arctic warms there is less sea ice on
average over the year. • Areas free of sea ice absorb heat instead
of reflect it. • This creates even more warming and
more ice melt. • Which results a positive feedback loop.
34
What about the oceans? Ocean versus land
Air above oceans versus ocean water
36
12/13/17
7
38
Energy Budget Inflation
"Looking for a Similar Assignment? Get Expert Help at an Amazing Discount!"
