Climate classifications Koppen// koppen climate classification of worldNarendranath Guria
Climate classifications Koppen, world climate classification, major climate region of world, climate zone of world, classification of world climate, koppen climate classification,
It is a presentation about the
Koppen's climate classification system. It provides an overview of Koppen system.It is an informative and engaging overview of the Koppen climate classification system, providing a useful resource for anyone interested in understanding how climate is classified and how it impacts different regions around the world.
Climate classifications Koppen// koppen climate classification of worldNarendranath Guria
Climate classifications Koppen, world climate classification, major climate region of world, climate zone of world, classification of world climate, koppen climate classification,
It is a presentation about the
Koppen's climate classification system. It provides an overview of Koppen system.It is an informative and engaging overview of the Koppen climate classification system, providing a useful resource for anyone interested in understanding how climate is classified and how it impacts different regions around the world.
This presentation is a summary about world climates addressed to my bilingual students in 3rd ESO. It consists of some information about the main climates together with representative pictures. It is a descriptve study.
Characterization and the Kinetics of drying at the drying oven and with micro...Open Access Research Paper
The objective of this work is to contribute to valorization de Nephelium lappaceum by the characterization of kinetics of drying of seeds of Nephelium lappaceum. The seeds were dehydrated until a constant mass respectively in a drying oven and a microwawe oven. The temperatures and the powers of drying are respectively: 50, 60 and 70°C and 140, 280 and 420 W. The results show that the curves of drying of seeds of Nephelium lappaceum do not present a phase of constant kinetics. The coefficients of diffusion vary between 2.09.10-8 to 2.98. 10-8m-2/s in the interval of 50°C at 70°C and between 4.83×10-07 at 9.04×10-07 m-8/s for the powers going of 140 W with 420 W the relation between Arrhenius and a value of energy of activation of 16.49 kJ. mol-1 expressed the effect of the temperature on effective diffusivity.
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
"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.
In-depth exploration of the carbon cycle reveals the delicate balance required to sustain life and the urgent need to address anthropogenic influences. Through research, education, and policy, we can work towards restoring equilibrium in the carbon cycle and ensuring a sustainable future for generations to come.
UNDERSTANDING WHAT GREEN WASHING IS!.pdfJulietMogola
Many companies today use green washing to lure the public into thinking they are conserving the environment but in real sense they are doing more harm. There have been such several cases from very big companies here in Kenya and also globally. This ranges from various sectors from manufacturing and goes to consumer products. Educating people on greenwashing will enable people to make better choices based on their analysis and not on what they see on marketing sites.
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.
Natural farming @ Dr. Siddhartha S. Jena.pptxsidjena70
A brief about organic farming/ Natural farming/ Zero budget natural farming/ Subash Palekar Natural farming which keeps us and environment safe and healthy. Next gen Agricultural practices of chemical free farming.
Artificial Reefs by Kuddle Life Foundation - May 2024punit537210
Situated in Pondicherry, India, Kuddle Life Foundation is a charitable, non-profit and non-governmental organization (NGO) dedicated to improving the living standards of coastal communities and simultaneously placing a strong emphasis on the protection of marine ecosystems.
One of the key areas we work in is Artificial Reefs. This presentation captures our journey so far and our learnings. We hope you get as excited about marine conservation and artificial reefs as we are.
Please visit our website: https://kuddlelife.org
Our Instagram channel:
@kuddlelifefoundation
Our Linkedin Page:
https://www.linkedin.com/company/kuddlelifefoundation/
and write to us if you have any questions:
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Alert-driven Community-based Forest monitoring: A case of the Peruvian Amazon
Koppen Climate Classification
1.
2. Introduction
• The close correlation between climate and vegetation is evident in
every part of the world.
• The strong connection between the two is also proving to play a key
role in categorizing and dividing the global climate into more specific
zones.
• Each climate zone is identified by its unique combination of vegetation,
temperature, and precipitation.
• These three variables are also determining factors in climate
classification.
• During the late 19th Century, climatologist Wladimir Köppen used
vegetation, temperature, and precipitation as the key components in
developing the Köppen Climate Classification.
3. Koppen Climate Classification
• The Köppen Climate Classification is a
widely-used classification system that
divides the global climate into five
climate zones primarily based on
vegetation.
• Developed by Wladimir Köppen at the
end of the 19th century, the system uses
precipitation and temperature as the two
key components to classify the climate of
a region, as they are the determining
factors for the type of vegetation that
occurs.
4. Explanation
• Late in the 19th century, climatologist and botanist Wladimir
Köppen developed a climate classification system based on
vegetation.
• He used the correlation between vegetation and climate in
different regions to divide the world's climate into specific
zones.
• The resulting Köppen Climate Classification categorizes the
global climate into five distinct zones, primarily based on the
temperature and precipitation experienced by each one.
• Köppen continued to change and refine his classification
system, with two of the most important amendments made in
1918 and 1936.
5. Climate Zones Of The World
• According to the Köppen Climate Classification, the global climate
can be divided into five primary zones. These climate zones are based
on regional vegetation and defined by the temperature and
precipitation that is responsible for its formation.
6. Cont.
• The zones are defined by the capital letters A, B, C, D, and E. The
climate zones defined by each letter are:
• A) Tropical Climates
• B) Dry Climates
• C) Temperate Climates
• D) Continental Climates
• E) Polar Climates
7. Tropical Climates
Tropical (also known as equatorial) climates occur in regions
situated around the equator and expand to latitudes of 15° to 25°
to the north and south. It can be defined by the following
characteristics:
It is the warmest of all the climate zones.
Regions in this zone have an average monthly temperature of higher
than 18° Celsius (64.4° Fahrenheit.)
Annual precipitation exceeds 1 500 millimeters in this zone.
High humidity levels and warm temperatures result in a frequent,
almost daily occurrences of cumulus or larger cumulonimbus cloud
formations.
8.
9. This zone is divided into three subcategories, which
are classified according to temperature and dryness.
• Af - Tropical Rainforest Climate (no dry season.)
• Am - Tropical Monsoon Climate (short dry season)
•Aw/As - Tropical Savanna Climate (winter dry
season)
10. Dry Climates
Dry (or arid) climates occur in regions situated at latitudes between 20°
to 35° north and south of the equator. It can be defined by the following
characteristics:
• The main feature of this climate zone is the complete absence or
extremely low levels of annual precipitation.
• The very dry atmospheric conditions are the result of the combined
evaporation and transpiration levels exceeding the total amount of
precipitation.
• Vegetation is sparse or completely absent as a result of the dry
climate with very little precipitation.
11.
12. Cont.
• This climate zone is divided into desert (BW) and semi-arid
(BS) regions, according to vegetation type. It is further
categorized into hot (h) and cold (k) zones:
• BWh - Hot Desert Climate
• BWk - Cold Desert Climate
• BSh - Hot Semi-Arid Climate
• BSk - Cold Semi-Arid Climate
13. Temperate Climates
Temperate (or mesothermal) climates occur
in regions situated at latitudes between 30° to
50° north and south of the equator. It can be
defined by the following characteristics:
• Regions in this climate zone typically
experience warm summers with high levels of
humidity and mild winter seasons.
• During the year, the warmest month is at least
10° Celsius (60° Fahrenheit) or higher, while
the coldest month is lower than 18° Celsius
(64.4° Fahrenheit) but higher than -3° Celsius
(26.6° Fahrenheit).
• These climate zones are typically located on
the edges of continents, along the eastern and
western coastlines.
14. Cont.
• Temperate climate zones are divided into three main categories
according to precipitation: mild temperate dry winters (Cw), mild
temperate dry summers (Cs), and mild temperate humid (Cf) climates.
All three subcategories are further divided according to temperatures:
• Cfa - Humid Subtropical Climate
• Cfb - Temperate Oceanic Climate
• Cfc - Subpolar Oceanic Climate
• Csa - Hot-Summer Mediterranean Climate
• Csb - Warm-summer Mediterranean
• Csc - Cold-summer Mediterranean Climate
• Cwa - Monsoon-Influenced Humid Subtropical Climate
• Cwb - Subtropical Highland Climate
• Cwc - Cold Subtropical Highland Climate
15. Continental Climates
Continental climates typically occur in regions situated at
latitudes between 40° and 75° north and south of the equator.
(Although this type of climate is rare in the Southern
Hemisphere.) It can be defined by the following characteristics:
• The average temperature of the warmest month is above 10°
Celsius (50° Fahrenheit), while the coldest month is below -3°
Celsius (26.6° Fahrenheit).
• This climate type is usually found in the interior of continents.
• Regions in this zone experience summers with warm to cool
temperatures, while the winters are generally cold.
16. Continental climate zones are divided into three main categories according
to precipitation: continental dry summer (Ds), continental dry winter (Dw),
and continental humid (Df) climates. Like temperate climates, they are
further divided according to temperature:
• Dfa - Hot-Summer Humid Continental Climate
• Dfb - Warm-Summer Humid Continental Climate
• Dfc - Subarctic Climate
• Dfd - Extremely Cold Subarctic Climate
• Dsa - Hot Dry-Summer Continental Climate
• Dsb - Warm Dry-Summer Continental Climate
• Dsc - Subarctic Climate
• Dsd - Very Cold Subarctic Climate
• Dwa - Monsoon-Influence Hot-Summer Humid Continental Climate
• Dwb - Monsoon-Influence Warm-Summer Humid Continental Climate
• Dwc - Monsoon-Influence Subarctic Climate
• Dwd - Monsoon-Influence Extremely Cold Subarctic Climate
17.
18. Polar Climates
Polar climates are located at latitudes above 70° over the Arctic,
Greenland, and Antarctica. It is characterized by its all-year-round cold
temperatures and little to no vegetation. The following characteristics
define it more precisely:
• The warmest month of the year is below 10° Celsius (50° Fahrenheit).
• Polar climate regions are extremely dry, with annual precipitation of less than 25
cm (10 inches).
19. Polar climates are divided into two categories according
to vegetation:
• ET - Tundra
• EF - Ice Cap Climate
Tundra Climates consist of very little vegetation (mainly
loose shrubs, mosses, and dwarf trees) over a surface
where the soil is frozen for several hundred meters. (A
condition known as permafrost.) Ice Cap Climates are
completely covered by ice or snow.
20. Conclusion
• As clearly illustrated throughout this article, several smaller
climate regions exist within each of the five major climate
zones. Vegetation, temperature, and precipitation have been
the key factors used in determining each subcategory.
• Most countries throughout the world experience multiple
sub-climates, and many larger regions are influenced by five
or more different climate types at any given time.