Regionaldistributionoftemperature bytanujpareek
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The document discusses temperature zones on Earth. According to ancient Greeks, there are three temperature zones based on latitude: the tropical zone between the Tropics of Cancer and Capricorn which has a consistent high temperature; the temperate zone between 23.5-66.5 degrees latitude which has seasonal variations; and the frigid zone near the poles which has consistently low temperatures. However, Soupan proposed determining temperature zones based on isotherms which take into account additional factors like continents, oceans, winds and ground surface.
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Climate
Climate is defined as the average weather in a region over a long period of time, typically 30 years. It is influenced by factors like latitude, altitude, proximity to bodies of water and oceans, and vegetation. There are several classification systems for climates, most commonly the Köppen system which categorizes climates as tropical, temperate, or polar. Tropical climates have high temperatures year-round, temperate climates have distinct seasons with moderate temperature changes, and polar climates are very cold with no warm summers. Paleoclimatology studies past climates through proxies like sediments and tree rings since direct observations are only available recently.
Heat zones of the earth (2)
The document discusses the five major latitude regions of the Earth's surface divided based on climate: the North and South Frigid Zones, the North and South Temperate Zones, and the Torrid Zone. These zones were first theorized by ancient Greek philosophers and later refined over time as geographic knowledge improved. Today, the most commonly used climate classification system divides the world into five climate zones based on factors like average temperature and precipitation.
world climates finale
The document discusses the composition and importance of Earth's atmosphere. It can be summarized as follows:
1) Earth's atmosphere is made up primarily of nitrogen and oxygen gases which support life by providing breathable air and nourishing plant growth.
2) The atmosphere also regulates Earth's climate and weather patterns through factors like temperature, precipitation, air pressure, and wind.
3) It protects the planet from harmful rays and materials from space while trapping heat via the greenhouse effect, maintaining a livable temperature range.
Earth's physical geo part 1
The document discusses how the Earth moves in space and why seasons change. It explains that the Earth rotates on its axis over 24 hours, causing day and night, and revolves around the Sun over the course of a year. The Earth's tilted axis and elliptical orbit cause the seasons, with regions facing the Sun more directly experiencing longer days and warmer temperatures. The document also describes the latitudinal zones of the tropics, temperate, and polar regions and how temperatures vary across these zones.
World Weather Types: Equatorial, Tropical, Desert, Mediterranean, Temperate a...
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The document summarizes different types of world weather and climate regions, including tropical, desert/dry, temperate, continental, and polar climates. It describes the key characteristics of each climate type, such as average temperatures, precipitation levels, seasonal patterns, and example regions that exhibit each climate. The document also discusses subcategories within tropical and desert climates.Climate zones
The Earth is divided into five climate zones based on temperature: two cool climate zones within the polar circles where the sun's rays hit obliquely and temperatures are always cold; two temperate zones between the tropics and polar circles where the sun's rays hit at a greater angle and temperatures are mild and vary seasonally; and a hot climate zone between the Tropic of Cancer and Capricorn where the sun's rays hit perpendicularly, temperatures are always high, and there is little seasonal variation.
Climate zones
The document divides the planet into five main climate zones - two cool climate zones within the polar circles which have cold temperatures all year round due to the sun's oblique angle, two temperate zones between the tropics and polar circles which have mild temperatures that vary seasonally, and one hot climate zone between the Tropic of Cancer and Capricorn which has always high temperatures with little seasonal difference due to the sun's perpendicular rays. Within each zone there are further divisions of specific climate types.
Earth sun relationship
The Earth-Sun relationship affects climate in the following ways:
1. The Earth's 23.5 degree tilt causes uneven heating and results in seasons as the tilt changes in relation to the Sun throughout the year.
2. The Tropics of Cancer and Capricorn mark the beginning of summer and winter in the Northern Hemisphere when the Sun's rays directly strike them.
3. Areas above 66.5 degrees north and south latitude experience extremes of 24 hours of daylight or darkness depending on the season.
CLIMATIC ZONES
This document discusses three main climatic zones: tropical, equatorial, and temperate. It provides characteristics of each zone. The tropical zone extends from 0-23.5 degrees latitude and has very warm temperatures due to high solar radiation. The subtropics from 23.5-40 degrees receive less moisture and have deserts. The temperate zone from 40-60 degrees has cooler average temperatures and distinct seasons compared to the other zones.
Latitudes and Longitudes
Rita and Gita are surprised to receive a letter from their friend Rahul in Singapore saying that Singapore is two hours ahead of India. They look at a globe to see the exact location of Singapore and see lines running across countries. The document goes on to explain that these lines are latitudes and longitudes, which help calculate the positions of countries and have been useful for explorers, the military, and pilots. It provides details on what a globe is, the axis and equator, hemispheres, parallels of latitude that run parallel to the equator, important parallels like the Tropics of Cancer and Capricorn, how latitude is measured, and heat zones on Earth based on latitude.
Climate
Earth's climate is influenced by its position relative to the sun, which affects factors like temperature, daylight hours, and seasons. Climate refers to long-term weather patterns typical of a region, while weather describes short-term atmospheric conditions. A variety of geographic factors, including latitude, elevation, ocean currents, prevailing winds, and landforms further impact regional climates. These combine to produce a wide diversity of climates around the world.
KOPPEN'S CLIMATE (Climate pattern of world)
Climate, climatic zones, Koppens climate classification of world, factor affecting climate changes.
useful for all graduate and postgraduate students.
Capter 5 Climate of Ethiopia and the Horn GeES 1011.pdf
Upon the completion of this chapter, you will be able to:
Distinguish between weather and climate,
Explain the place to place distribution of temperature and rainfall in Ethiopia,
explain the time to time patterns of temperature and rainfall in Ethiopia,
Analyze climate and its implications on biophysical and socioeconomic aspects,
identify the causes, consequences and response mechanisms of climate change.
5.1 The concept of weather and climate
Both weather and climate are concepts about atmospheric conditions. The basic difference on them is duration and areal coverage.
Weather is atmospheric condition observed in a very specific area with a short term fluctuation, while
Climate is a prolonged(30-35years) atmospheric condition observed in a relatively wider geographic area.
Weather condition likely changed hour to hour, in a daily base or weakly but climate is relatively permanent.
Elements of Weather and Climate
Elements(components) of weather and climate are the following variables
Atmospheric temperature (how cold or hot is the atmosphere)
Precipitation (any kind of moisture falling from the atmosphere to the ground, mostly rainfall)
Air pressure (the weight exerted by the air)
Humidity (the level or proportion of water vapor within the atmosphere)
Sunshine (the duration and intensity of solar heat as well as light)
Wind (horizontal motion of air)
Unit 3 weather and climate wiki
This document provides an overview of weather and climate elements and factors, including temperature, humidity, precipitation, atmospheric pressure, and wind. It then describes the major climate types around the world, grouping them into hot climates near the equator, temperate climates between the tropics and polar circles, and cold polar climates. Specific climate types discussed include equatorial, tropical, desert, Mediterranean, continental, oceanic, subtropical, polar, and alpine. Maps and diagrams are referenced to help identify the locations and characteristics of different climates.
FACTORS AFFECTING CLIMATE IN SPECIFIC AREA
The document discusses several key factors that affect climate:
1. Latitude - Places closer to the equator receive more direct sunlight and have a warmer climate, while areas farther from the equator have a colder climate due to the sun's rays striking at a lower angle.
2. Altitude - Higher elevations have lower air pressure and temperature, with air temperature decreasing approximately 6.5°C for every 1000 meters gained in elevation.
3. Distance from large bodies of water - Oceans and seas moderate nearby climate by slowly absorbing and releasing heat, preventing large fluctuations in air temperature.
G9 Science Q3- Week 4_5- Factors that affect Climate.ppt
Six factors that affect climate are identified: latitude, proximity to large bodies of water, topography, elevation, atmospheric circulation, and vegetation. Latitude determines average annual temperature, with temperatures decreasing as latitude increases. Proximity to water moderates temperatures, resulting in cooler summers and milder winters. Topography such as mountains can cause a rain shadow effect with wetter windward sides and drier leeward sides. Higher elevations experience lower average annual temperatures. Atmospheric circulation distributes heat and moisture globally. Vegetation influences temperature absorption and precipitation patterns through transpiration.
Koppen Climate Classification
in this Presentation we will learn about the five zones of climate in different regions. for further information let seee the Presentation.
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Beige Brown Vintage Group Project Presentation.pdf
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World Weather Types: Equatorial, Tropical, Desert, Mediterranean, Temperate a...
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More from Tanuj Joshi
Salinity and it's distribution
This document discusses salinity and its distribution in the oceans. It defines salinity as the amount of dissolved solid material in water, typically expressed in parts per thousand. The main constituents that determine ocean salinity are chloride, sodium, sulfate and magnesium. Salinity varies in different locations from around 33-38‰ in the open ocean to over 300‰ in places like the Dead Sea. Processes like evaporation and ice formation increase salinity while precipitation and melting decrease it. Global patterns of surface salinity are also discussed, with lower salinity at high latitudes and higher salinity in the tropics.
Ocean currents (pacific)
The document summarizes several ocean currents in the Pacific Ocean. It describes how surface currents are driven by prevailing winds and form large gyres that rotate clockwise in the north and counterclockwise in the south. In the North Pacific, the surface circulation is dominated by a clockwise-rotating gyre formed by the North Equatorial Current, Kuroshio Current, North Pacific Current, and California Current. In the South Pacific, the surface circulation is dominated by a counterclockwise-rotating gyre formed by the South Equatorial Current, East Australia Current, northern edge of the West Wind Drift, and Peru Current. The document also provides details on several specific currents including the North Equatorial Current, Oy
Temperature and it’s distribution(ocean)
This document discusses the horizontal and vertical distribution of temperature in oceans. It notes that ocean temperatures are highest at the equator (26.7°C on average) and decrease towards the poles. Factors like latitude, ocean currents, prevailing winds, local weather, and depth influence ocean temperatures. Temperature decreases with depth but not uniformly, dropping more rapidly in the top 200m (photic zone) and leveling off below 2000m. The thermocline zone between 300-1000m marks the transition between warmer surface waters and colder deeper waters.
Ocean Currents
The document summarizes ocean currents. It discusses that surface currents are driven by prevailing winds in predictable patterns, though the motion of water continues due to inertia even without wind. It describes the major ocean gyres like the counterclockwise rotating gyre in the Indian Ocean formed by currents like the South Equatorial Current. It also discusses the Arctic Ocean's large clockwise gyre displaced toward the Canadian Basin and water flowing out of the Arctic into the North Atlantic. Eddies are discussed as currents sometimes closing in on themselves. Global circulation patterns have changed over time in response to shifting continents and climate.
Temperature and its vertical distribution in ocean water
1. There are typically three layers of ocean water from the surface to the bottom in tropical regions based on temperature: a warm top layer about 500m thick, a thermocline layer below it with rapidly decreasing temperatures, and a very cold third layer extending to the ocean floor.
2. Temperature decreases with depth but the rate is not uniform. Below 2000m the change is negligible. Near the poles there is generally just one cold layer throughout. Factors like latitude, winds, currents influence horizontal and vertical temperature distributions.
3. Vertically, oceans have an upper euphotic zone to 200m depth receiving solar radiation, and an aphotic zone below it. The thermocline separates the warm
Enso
The document discusses the El Niño Southern Oscillation (ENSO), a recurring climate pattern involving changes in the temperature of waters in the eastern tropical Pacific Ocean. ENSO involves shifts between El Niño (warm) and La Niña (cool) phases that impact weather worldwide. It was discovered in the late 19th century by Gilbert Walker and involves changes in ocean temperatures, winds, and air pressure across the Pacific. Developing countries dependent on agriculture and fishing are most affected by the extremes in weather caused by ENSO.
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Regionaldistributionoftemperature bytanujpareek
- 1. BY:-TANUJ PAREEK Professional PPT Maker
- 2. The intensity of hotness or coldness of any substance is called Temperature. OR Degree of hotness of any object is called Temperature.
- 4. According to ancient Greek thinkers the globe is divided into three temperature zones on the basis of latitudes.
- 9. Tropical Zone extends between the tropics of Cancer(23.5˚ N) and Capricorn(23.5˚S). The sun’s rays are more or less vertical on equator throughout the year.
- 10. There is no winter around the equator because of high temperature prevailing throughout the year but as one approaches the tropics of Cancer and Capricorn summer and winter are clearly observed and differentiated.
- 11. Temperate Zone extends between 23.5˚ and 66.5 ˚ latitudes in both the hemispheres. Though the duration of day and night is no longer in this zone but it is never more than 24 Hours There are marked seasonal contrasts with the northward and southward(summer and winter solstices) migration of the overhead sun and thus range of temperature between summers and winters becomes exceptionally very high.
- 12. Frigid Zone extends between 66.5 ˚ latitudes and the poles in the hemispheres is characterized by more oblique sun’s rays throughout the year resulting into exceptionally very low temperature. The length of day and night is more than 24 hours. Day and nights are of 6 months duration at poles.
- 13. Sun is never vertical and the ground is covered with snow as temperature more or less remains below freezing point.
- 16. It may be pointed out that the Greeks gave undue importance to latitudes in determining different temperature zones and overlooked the controls of contrasting nature of continents and oceans in terms of their heating and cooling, prevailing winds, oceans
- 17. currents, nature of ground surface etc.Taking all these factors in consideration Soupan divided the globe into temperature zones on the basis of isotherms. According to him the outer limit of tropical zone should be determined on the basis of
- 18. annual isotherm of 68 ˚ F (20 ˚ C).The boundary between temperate and frigid zones in the northern hemisphere should be demarcated by 50 ˚F(10 ˚ C) isotherm of July while January isotherm of 50 ˚C(10 ˚ C) should separate temperate zone from the frigid zone in the southern hemisphere.