MEVE 011 Solved Assignment 2021-22
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Assignment 2022 , FREE MEVE 011 Assignment , IGNOU Assignments 2021-22- Gandhi
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MEVE 011 Solved Assignment 2021-22: for college kids – MEVE 011 GLOBAL
CLIMATE CHANGE Solved Assignment 2021-22, Students are advised that
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MEVE 011 Solved
Assignment 2021-22
Course Code : MEVE 011
Course Title : GLOBAL CLIMATE CHANGE
Assignment Code : MEVE 011/TMA-01/2021
Coverage : All Blocks
Maximum Marks 100 Attempt all questions. All questions
carry equal marks.
Attempt all questions. All questions
carry equal marks.
Note: This assignment is based on the
entire course. Answer any five questions. All question carries equal marks. The
marks for each question are indicated against it within brackets on the
right-hand side. Please write all answers in your own words.
1. Write short notes on the
following: (20 marks)
a. Structure of the atmosphere
Troposphere
The
troposphere is the atmospheric layer closest to the planet and contains the
largest percentage (around 80%) of the mass of the total atmosphere.
Temperature and water vapor content in the troposphere decrease rapidly with
altitude. Water vapor plays a major role in regulating air temperature because
it absorbs solar energy and thermal radiation from the planet's surface. The
troposphere contains 99 % of the water vapor in the atmosphere. Water vapor
concentrations vary with latitude. They are greatest above the tropics, where
they may be as high as 3 %, and decrease toward the polar regions.
All weather phenomena
occur within the troposphere, although turbulence may extend into the lower
portion of the stratosphere. Troposphere means "region of mixing" and
is so named because of vigorous convective air currents within the layer.
The upper
boundary of the layer, known as the tropopause, ranges in height from 5
miles (8 km) near the poles up to 11 miles (18 km) above the equator. Its
height also varies with the seasons; highest in the summer and lowest in the
winter.
Stratosphere
The
stratosphere is the second major strata of air in the atmosphere. It extends
above the tropopause to an altitude of about 30 miles (50 km) above the
planet's surface. The air temperature in the stratosphere remains relatively
constant up to an altitude of 15 miles (25 km). Then it increases gradually to
up to the stratopause. Because the air temperature in the stratosphere
increases with altitude, it does not cause convection and has a stabilizing
effect on atmospheric conditions in the region. Ozone plays the major role in
regulating the thermal regime of the stratosphere, as water vapor content
within the layer is very low. Temperature increases with ozone concentration.
Solar energy is converted to kinetic energy when ozone molecules absorb
ultraviolet radiation, resulting in heating of the stratosphere.
The ozone
layer is centered at an altitude between 10-15 miles (15-25 km). Approximately
90 % of the ozone in the atmosphere resides in the stratosphere. Ozone
concentration in the this region is about 10 parts per million by volume (ppmv)
as compared to approximately 0.04 ppmv in the troposphere. Ozone absorbs the
bulk of solar ultraviolet radiation in wavelengths from 290 nm - 320 nm (UV-B
radiation). These wavelengths are harmful to life because they can be absorbed
by the nucleic acid in cells. Increased penetration of ultraviolet radiation to
the planet's surface would damage plant life and have harmful environmental
consequences. Appreciably large amounts of solar ultraviolet radiation would
result in a host of biological effects, such as a dramatic increase in cancers.
Thermosphere
The
thermosphere is located above the mesosphere. The temperature in the
thermosphere generally increases with altitude reaching 600 to 3000 F (600-2000
K) depending on solar activity. This increase in temperature is due to the
absorption of intense solar radiation by the limited amount of remaining
molecular oxygen. At this extreme altitude gas molecules are widely separated.
Above 60 miles (100 km) from Earth's surface the chemical composition of air
becomes strongly dependent on altitude and the atmosphere becomes enriched with
lighter gases (atomic oxygen, helium and hydrogen). Also at 60 miles (100 km)
altitude, Earth's atmosphere becomes too thin to support aircraft and vehicles
need to travel at orbital velocities to stay aloft. This demarcation between
aeronautics and astronautics is known as the Karman Line. Above about 100
miles (160 km) altitude the major atmospheric component becomes atomic oxygen.
At very high altitudes, the residual gases begin to stratify according to
molecular mass, because of gravitational separation.
Exosphere
The
exosphere is the most distant atmospheric region from Earth's surface. In the
exosphere, an upward travelling molecule can escape to space (if it is moving
fast enough) or be pulled back to Earth by gravity (if it isn't) with little
probability of colliding with another molecule. The altitude of its lower
boundary, known as the thermopause or exobase, ranges from about
150 to 300 miles (250-500 km) depending on solar activity. The upper boundary
can be defined theoretically by the altitude (about 120,000 miles, half the
distance to the Moon) at which the influence of solar radiation pressure on
atomic hydrogen velocities exceeds that of the Earth's gravitational pull. The
exosphere observable from space as the geocorona is seen to extend to
at least 60,000 miles from the surface of the Earth. The exosphere is a
transitional zone between Earth's atmosphere and interplanetary space.
b. Radiative forcing
2. Write short notes on the
following: (20 marks)
a. Anthropogenic drivers of climate
change
b. “Cloud feedback” and “Lapse-rate
feedback”
3. Explain the sources of
palaeoclimatic data. (20 marks)
4. Explain the direct and indirect
effects of climate change on agriculture. (20 marks)
5. Explain the impacts of climate
change on human health. (20 marks)
6. Write short notes on the
following: (20 marks)
a. Glacier Lake Outburst floods
b. Paris Agreement
7. Explain the National Action Plan
on Climate change. (20 marks)
8. Write short notes on the
following: (20 marks)
a. Concept of mitigation and
adaptation
b. UNFCCC
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MEVE 011 GLOBAL CLIMATE CHANGE Solved
Assignment 2021-22: Those students who had
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Assignment 2021-22 All this is often available in a web mode. After
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Those students who had
successfully submitted their Assignments to their allocated study centres can
now check their Assignment Status. Along with assignment status, they can also
checkout their assignment marks & result. MEVE 011 Solved
Assignment 2021-22 All this is available in an online mode. MEVE
011 Solved Assignment 2021-22 After submitting the assignment, you can
check you IGNOU Assignment Status only after 3-4 weeks. It might take 40 days
to declare.
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Assignment 2021-22 Here the students can check their IGNOU Assignment
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