This presentation contains about the layers of the atmosphere which has 5 layers in atmosphere
The first layer is troposphere
The second layer is stratosphere
The third layer is mesosphere
The fourth layer is ionosphere and
The fifth layer is exosphere
green house effect(power point presentation)
prepared by :rishabh sood
school:k.v palampur
class:11th science
from:palampur(h,p)
for more contact:rishabhsood92@gmail.com
This presentation contains about the layers of the atmosphere which has 5 layers in atmosphere
The first layer is troposphere
The second layer is stratosphere
The third layer is mesosphere
The fourth layer is ionosphere and
The fifth layer is exosphere
green house effect(power point presentation)
prepared by :rishabh sood
school:k.v palampur
class:11th science
from:palampur(h,p)
for more contact:rishabhsood92@gmail.com
Importance of Atmosphere –
Physical and chemical characteristics of Atmosphere –
Vertical structure of the atmosphere –
Composition of the atmosphere –
Temperature profile of the atmosphere –
Lapse rates –
Temperature inversion –
Effects of inversion on pollution dispersion.
Atmospheric stability
Earth’s atmosphere is a thin blanket of gases and tiny particles — together called air.
Atmosphere is the air surrounding the earth.
The Earth’s atmosphere is a mixture of gases and water vapour, and also of some amount of aerosols (dust, smoke, condensation products of vapor)
It contains life-giving gases like Oxygen for humans and animals and carbon dioxide for plants.
It envelops the earth all round and is held in place by the gravity of the earth.
It helps in stopping the ultraviolet rays harmful to the life and maintains the suitable temperature necessary for life.
power point presentation in atmospheric chemistryJamaicaFiel
this will provide quick discussion on atmospheric chemistry and some other details on atmosphere including layers of the atmosphere and environmental problems in the atmosphere
Chapter 4THE ATMOSPHERE14.1 THE ATMOSPHERE4.1.1 .docxchristinemaritza
Chapter 4
THE ATMOSPHERE
1
4.1 THE ATMOSPHERE
4.1.1 INTRODUCTION
The atmosphere, the gaseous layer that surrounds the earth, formed over four billion years ago. During
the evolution of the solid earth, volcanic eruptions released gases into the developing atmosphere. Assuming
the outgasing was similar to that of modern volcanoes, the gases released included: water vapor (H2O),
carbon monoxide (CO), carbon dioxide (CO2), hydrochloric acid (HCl), methane (CH4), ammonia (NH3),
nitrogen (N2) and sulfur gases. The atmosphere was reducing because there was no free oxygen. Most of
the hydrogen and helium that outgassed would have eventually escaped into outer space due to the inability
of the earth's gravity to hold on to their small masses. There may have also been signi�cant contributions
of volatiles from the massive meteoritic bombardments known to have occurred early in the earth's history.
Water vapor in the atmosphere condensed and rained down, eventually forming lakes and oceans. The
oceans provided homes for the earliest organisms which were probably similar to cyanobacteria. Oxygen
was released into the atmosphere by these early organisms, and carbon became sequestered in sedimentary
rocks. This led to our current oxidizing atmosphere, which is mostly comprised of nitrogen (roughly 71
percent) and oxygen (roughly 28 percent). Water vapor, argon and carbon dioxide together comprise a
much smaller fraction (roughly 1 percent). The atmosphere also contains several gases in trace amounts,
such as helium, neon, methane and nitrous oxide. One very important trace gas is ozone, which absorbs
harmful UV radiation from the sun.
4.1.2 ATMOSPHERIC STRUCTURE
The earth's atmosphere extends outward to about 1,000 kilometers where it transitions to interplanetary
space. However, most of the mass of the atmosphere (greater than 99 percent) is located within the �rst
40 kilometers. The sun and the earth are the main sources of radiant energy in the atmosphere. The
sun's radiation spans the infrared, visible and ultraviolet light regions, while the earth's radiation is mostly
infrared.
The vertical temperature pro�le of the atmosphere is variable and depends upon the types of radiation
that a�ect each atmospheric layer. This, in turn, depends upon the chemical composition of that layer
(mostly involving trace gases). Based on these factors, the atmosphere can be divided into four distinct
layers: the troposphere, stratosphere, mesosphere, and thermosphere.
The troposphere is the atmospheric layer closest to the earth's surface. It extends about 8 - 16 kilometers
from the earth's surface. The thickness of the layer varies a few km according to latitude and the season of
the year. It is thicker near the equator and during the summer, and thinner near the poles and during the
1This content is available online at <http://cnx.org/content/m16687/1.2/>.
Available for free at Connexions <http://cnx.org/content/col10548/1.2>
15
16 CHAPTER 4. THE ATMOS ...
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Climate Change All over the World .pptxsairaanwer024
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Prevalence of Toxoplasma gondii infection in domestic animals in District Ban...Open Access Research Paper
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UNDERSTANDING WHAT GREEN WASHING IS!.pdfJulietMogola
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"Understanding the Carbon Cycle: Processes, Human Impacts, and Strategies for...MMariSelvam4
The carbon cycle is a critical component of Earth's environmental system, governing the movement and transformation of carbon through various reservoirs, including the atmosphere, oceans, soil, and living organisms. This complex cycle involves several key processes such as photosynthesis, respiration, decomposition, and carbon sequestration, each contributing to the regulation of carbon levels on the planet.
Human activities, particularly fossil fuel combustion and deforestation, have significantly altered the natural carbon cycle, leading to increased atmospheric carbon dioxide concentrations and driving climate change. Understanding the intricacies of the carbon cycle is essential for assessing the impacts of these changes and developing effective mitigation strategies.
By studying the carbon cycle, scientists can identify carbon sources and sinks, measure carbon fluxes, and predict future trends. This knowledge is crucial for crafting policies aimed at reducing carbon emissions, enhancing carbon storage, and promoting sustainable practices. The carbon cycle's interplay with climate systems, ecosystems, and human activities underscores its importance in maintaining a stable and healthy planet.
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Willie Nelson Net Worth: A Journey Through Music, Movies, and Business Venturesgreendigital
Willie Nelson is a name that resonates within the world of music and entertainment. Known for his unique voice, and masterful guitar skills. and an extraordinary career spanning several decades. Nelson has become a legend in the country music scene. But, his influence extends far beyond the realm of music. with ventures in acting, writing, activism, and business. This comprehensive article delves into Willie Nelson net worth. exploring the various facets of his career that have contributed to his large fortune.
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Introduction
Willie Nelson net worth is a testament to his enduring influence and success in many fields. Born on April 29, 1933, in Abbott, Texas. Nelson's journey from a humble beginning to becoming one of the most iconic figures in American music is nothing short of inspirational. His net worth, which estimated to be around $25 million as of 2024. reflects a career that is as diverse as it is prolific.
Early Life and Musical Beginnings
Humble Origins
Willie Hugh Nelson was born during the Great Depression. a time of significant economic hardship in the United States. Raised by his grandparents. Nelson found solace and inspiration in music from an early age. His grandmother taught him to play the guitar. setting the stage for what would become an illustrious career.
First Steps in Music
Nelson's initial foray into the music industry was fraught with challenges. He moved to Nashville, Tennessee, to pursue his dreams, but success did not come . Working as a songwriter, Nelson penned hits for other artists. which helped him gain a foothold in the competitive music scene. His songwriting skills contributed to his early earnings. laying the foundation for his net worth.
Rise to Stardom
Breakthrough Albums
The 1970s marked a turning point in Willie Nelson's career. His albums "Shotgun Willie" (1973), "Red Headed Stranger" (1975). and "Stardust" (1978) received critical acclaim and commercial success. These albums not only solidified his position in the country music genre. but also introduced his music to a broader audience. The success of these albums played a crucial role in boosting Willie Nelson net worth.
Iconic Songs
Willie Nelson net worth is also attributed to his extensive catalog of hit songs. Tracks like "Blue Eyes Crying in the Rain," "On the Road Again," and "Always on My Mind" have become timeless classics. These songs have not only earned Nelson large royalties but have also ensured his continued relevance in the music industry.
Acting and Film Career
Hollywood Ventures
In addition to his music career, Willie Nelson has also made a mark in Hollywood. His distinctive personality and on-screen presence have landed him roles in several films and television shows. Notable appearances include roles in "The Electric Horseman" (1979), "Honeysuckle Rose" (1980), and "Barbarosa" (1982). These acting gigs have added a significant amount to Willie Nelson net worth.
Television Appearances
Nelson's char
WRI’s brand new “Food Service Playbook for Promoting Sustainable Food Choices” gives food service operators the very latest strategies for creating dining environments that empower consumers to choose sustainable, plant-rich dishes. This research builds off our first guide for food service, now with industry experience and insights from nearly 350 academic trials.
8. Lowest and densest layer of the atmosphere.
Extends upto height 16kms =equator, 8kms = poles
All weather phenomena occur in troposphere.
Contains dust particles & water vapour.
Temp falls with increase in height.
9.
10. 2nd layer of the atmosphere.
Average altitude= 11 to 50 kms.
Most of the ozone is contained here.
Meteors entering the earth’s atmosphere get burnt here.
Long distance aircrafts fly in lower part of this layer.
11.
12. 3rd layer of the atmosphere.
Occurs between stratosphere and thermosphere.
Lies 50-80 Km above the Earth’s surface.
Coldest atmospheric layer.
Temp falls with elevation in this layer.
Meteors burns while entering the Earth’s atmosphere.
13.
14. 4th layer of the atmosphere.
Lies 80-600 Km above the Earth’s surface.
Located highest above the Earth’s surface.
Hottest layer in the atmosphere.
23. DEPLETION IN OZONE LAYER
• Chlorofluorocarbons (CFC) have caused a severe damage in
ozone layer.
• The main cause of ozone depletion and the ozone hole is
manufactured chemicals, especially manufactured halocarbon
refrigerants, solvents, propellants and foam-blowing agents
(chlorofluorocarbons (CFCs), (HCFCs), (HALONs), referred to
as ozone-depleting substances (ODS).
24. Green house effect
Natural warming process.
Carbon di-oxide and other gases are always present in the
atmosphere.
Human activities such as burning of fossil fuels and clear-cutting
of forests. , have accelerated the greenhouse effect and
caused GLOBAL WARMING
27. Global warming is the long-term heating of
Earth's climate system, due to human activities, such as fossil
fuel burning, which increases heat-trapping greenhouse gas
levels in Earth's atmosphere.
28. WAYS TO REDUCE GLOBAL WARMING
Plant more trees.
Reduce, Reuse, Recycle.
Use Less Heat and Air Conditioning.
Change your light-bulbs.
Use Solar vehicles.
Buy Energy-Efficient Products.
Use Less Hot Water.