Lecture 4: Global Warming and the Greenhouse Effect Flashcards

1
Q

What is the greenhoues effect?

A

Some sunlight that hits the earth is reflected, some becomes heat. Greenhouse gases in the atmosphere trap heat, keeping the earth warm.

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2
Q

What are the greenhouse gases?

A

Carbon dioxide, methane, nitrous oxide, CFC (chloro fluoro carbons)

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3
Q

Basic elements of the global warming problem

A
  1. Emissions of greenhouse gases
  2. increases in the atmospheric concentration
  3. increase in radiative forcing
  4. increases in average temperature
  5. Changes in global climate
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4
Q

Stefan boltzman law:

A

Q max = sigma * A * T^4

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5
Q

Climate vs weather

A

Climate is the average weather conditions of a place over a long period of time
Weather is the day to day conditions of the earth’s atmosphere at a particular place and time

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6
Q

What fraction of the outgoin radiation form the earth is blocked by the atmosphere?

A

around 30% of the solar radiation is reflected by the atmosphere, 70% is absorbed.

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7
Q

Troposhere

A

80% of gases
drives substantial air mixing. and movements
temp lowers are you go up

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8
Q

strato sphere

A

protective ozone layer, increasing temp with altitude

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9
Q

Greenhouse effect:

A

If we were to increase the concentration of gases such as CO2
, CH4
, N2O, and H2O in the
atmosphere ➔more absorption ➔ making the atmosphere’s ratio of outgoing to incoming
transparency decline.
• In turn, the average temperature of the earth would rise, thus producing the so-called greenhouse
effect.
• The group consisting of CO2
, CH4
, N2O, etc. are collectively called greenhouse gases

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10
Q

Indicators of global warming

A
Global temperature rise
warming oceans
shrinking ice sheets, glacia retreat
sea level rise
extreme weather
ocean acidification
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11
Q

1) Global temperature rise:

A

• Earth’s average surface temperature has risen about 0.9 degrees Celsius since the late
19th century, a change driven largely by increased CO2 and other anthropogenic
emissions into the atmosphere.
• Most of the warming occurred in the past 35 years

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12
Q

2) Warming oceans

A

The oceans have absorbed much of this increased heat, with the top 700 meters
(about 2,300 feet) of ocean showing warming of 0.302 degrees Fahrenheit since
1969
• The warming of the oceans has widespread effects. -
→ It causes marine heat waves that kill fish and coral reefs, fuels hurricanes and
coastal downpours, spawns harmful toxin-producing algal blooms

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13
Q

3) Shrinking ice sheets, glacial retreat

A

Mountain glaciers all over the world are in retreat.

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14
Q

4) sea level rise

A

• Melting ice sheets and glaciers
• Expansion of seawater with temperature increase
• Global sea level rose about 8 inches in the last century. The rate in the last two decades is
nearly double that of the last century.

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15
Q

5) extreme weather

A

Heat waves
• Drought
• Heavy downpours
→ The increase in evaporation (fairly uniform globally) implies an increase in precipitation (not
uniform), because the atmosphere can’t store water vapor indefinitely
• Floods
• Hurricanes
• Increased winter storm in Easter North America

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16
Q

6) ocean acidification

A

Ocean acidification is the ongoing decrease in the pH of the Earth’s oceans, caused by the uptake
of CO2
from the atmosphere.
• Seawater is slightly basic (meaning pH > 7), and ocean acidification involves a shift towards pHneutral conditions rather than a transition to acidic conditions (pH < 7).
• An estimated 30–40% of the carbon dioxide from human activity released into the atmosphere
dissolves into oceans, rivers and lakes. Some of it reacts with the water to form carbonic acid

17
Q

CO2 Emissions and energy use

A

Most of the energy used throughout the world is in the form of fossil fuels: oil, coal and
natural gas.
• Fossil fuels supply energy for transportation and industrial processes.
• Fossil fuels account for 75 % of the world’s annual energy consumption

18
Q

The lifetime of Greenhouse gases

A

THe atmospheric concentration of GHG will undergo an exponetial decay. THe longer the atmospheric lifetime, the slower and more gradual the depletion

19
Q

stabilization scenarios

A

They show how atmospheric CO2 concentrations migh tbe stablilized at levels from 450 to 1000 ppmv CO2. THis process is assuemd to take 75 -400 years, and it requires a substantial reduction in anthropogenic CO2