Q 1 – Which two climatic variables are used by Koeppen for classification of the climate?
Ans. It is an empirical classification based on the variables mean annual and mean monthly temperature and precipitation data. He introduced the use of capital and small letters to designate climatic groups and types. Although developed in 1918 and modified over a period of time, Koeppen’s scheme is still popular and in use. Koeppen recognised five major climatic groups, four of them are based on temperature and one on precipitation. Koeppen identified a close relationship between the distribution of vegetation and climate. He selected certain values of temperature and precipitation and related them to the distribution of vegetation and used these values for classifying the climates.
Q 2 – How is the “genetic” system of classification different from the “empirical one”?
Ans. Empirical classification is based on observed data, particularly on temperature and precipitation while genetic classification attempts to organise climates according to their causes
Q 3 – Which types of climates have very low range of temperature?
Ans. Tropical wet climate has very low range of temperature. It is found near the equator. The major areas are the Amazon Basin in South America, western equatorial Africa and the islands of East Indies. Significant amount of rainfall occurs in every month of the year as thunder showers in the afternoon. The temperature is uniformly high and the annual range of temperature is negligible. The maximum temperature on any day is around 30°C while the minimum temperature is around 20°C.
Tropical evergreen forests with dense canopy cover and large biodiversity are found in this climate.
Q 4 – What type of climatic conditions would prevail if the sun spots increase?
Ans. Sunspots are dark and cooler patches on the sun which increase and decrease in a cyclical manner. According to some meteorologists, when the number of sunspots increase, cooler and wetter weather and greater storminess occur. A decrease in sunspot numbers is associated with warm and drier conditions.
Q 5 – What type of vegetation would you find in the “C” and “A” type(s) of climate?
Ans. Group A: Tropical Humid Climates Tropical humid climates exist between Tropic of Cancer and Tropic of Capricorn. The sun being overhead climate hot and humid. Annual range of temperature is very low and annual rainfall is high. The tropical group is divided into three types, namely:
- Af- Tropical wet climate;
- Am – Tropical monsoon climate;
- Aw- Tropical wet and dry climate.
Group C: Warm temperate (mid-throughout the year and the presence of Inter Tropical Convergence Zone (ITCZ) make the latitude) climates extend from 30° – 50° of latitude mainly on the eastern and western margins of continents. These climates generally have warm summers with mild winters. They are grouped into four types:
- Humid subtropical, i.e. dry in winter and hot in summer (Cwa);
- Mediterranean (Cs);
- Humid subtropical, i.e. no dry season and mild winter (Cfa);
- Marine west coast climate (Cfb).
Q 6 – What do you understand by the term “Greenhouse Gases”? Make a list of greenhouse gases.
Ans. The term greenhouse is derived from the analogy to a greenhouse used in cold areas for preserving heat. A greenhouse is made up of glass. The glass which is transparent to incoming short wave solar radiation is opaque to outgoing long wave radiation. The glass, therefore, allows in more radiation and prevents the long wave radiation going outside the glass house, causing the temperature inside the glasshouse structure warmer . than outside.
Greenhouse gases are those gases which cause global warming and result in rise in atmospheric temperature. These gases absorb long wave radiation. The processes that warm the atmosphere are often collectively referred to as the greenhouse effect.
Greenhouse Gases(GHGs): The primary GHGs of concern today are carbon dioxide (C02), Chlorofluorocarbons (CFCs), methane (CH4), nitrous oxide (N20) and ozone (03). Some other gases such as nitric oxide (NO) and carbon monoxide (CO) easily react with GHGs and affect their concentration in the atmosphere. The effectiveness of any given GHG molecule will depend on the magnitude of the increase in its concentration, its life time in the atmosphere and the wavelength of radiation that it absorbs.
Q 7 – In how many categories can we classify type- A climate according to Koeppen?
Ans. The tropical group i.e. group- A is divided into three types, namely
- Af- Tropical wet climate;
- Am – Tropical monsoon climate;
- Aw- Tropical wet and dry climate.
Q 8 – In how many groups has Koeppen classified the climate?
Ans. Koeppen has classified climate into five groups: four are based on temperature and one is based on humidity. The capital letters: A, C, D and E delineate humid climates and B dry climates.
Q 9 – In which areas is tropical climate found? What are its features?
Ans. Tropical humid climates exist between Tropic of Cancer and Tropic of Capricorn. The sun being overhead throughout the year and the presence of Inter Tropical Convergence Zone (ITCZ) make the climate hot and humid. Annual range of temperature is very low and annual rainfall is high.
Q 10 – What is the astronomical theory of Millankovitch oscillations?
Ans. It is an astronomical theory of Millankovitch oscillations, which infer cycles in the variations in the earth’s orbital characteristics around the sun, the wobbling of the earth and the changes in the earth’s axial tilt. All these alter the amount of insolation received from the sun, which in turn, might have a bearing on the climate.
Q 11 – How does volcano affect the climate?
Ans. Volcanic eruption throws up lots of aerosols into the atmosphere. These aerosols remain in the atmosphere for a considerable period of time reducing the sun’s radiation reaching the Earth’s surface. After the recent Pinatoba and El Cion volcanic eruptions, the average temperature of the earth fell to some extent for some years.
Q 12 – Explain about tundra climate.
Ans. The tundra climate (ET) is so called after the types of vegetation, like low growing mosses, lichens and flowering plants. This is the region of permafrost where the sub soil is permanently frozen. The short growing season and water logging support only low growing plants. During summer, the tundra regions have very long duration of day light.
Q 13 – Explain about humid subtropical climate.
Ans. Humid subtropical climate occurs poleward of Tropic of Cancer and Capricorn, mainly in North Indian plains and South China interior plains. The climate is similar to Aw climate except that the temperature in winter is warm.
Q 14 – What is Kyoto Protocol?
Ans. International efforts have been initiated for reducing the emission of GHGs into the atmosphere. Kyoto protocol is the most important and was proclaimed in 1997. This protocol went into effect in 2005, ratified by 141 nations. Kyoto protocol bounds the 35 industrialised countries to reduce their emissions by the year 2012 to 5 per cent less than the levels prevalent in the year 1990.
Q 15 – In how many groups has warm temperate climates been divided?
Ans. They are grouped into four types:
- Humid subtropical, i.e. dry in winter and hot in summer (Cwa);
- Mediterranean (Cs);
- Humid subtropical, i.e. no dry season and mild winter (Cfa);
- Marine west coast climate (Cfb).
Q 16 – In which areas do we find tropical humid (Af) climate? What are its features?
Ans. Tropical wet climate is found near the equator. The major areas are the Amazon Basin in South America, western equatorial Africa and the islands of East Indies.
Features:
- Significant amount of rainfall occurs in every month of the year as thunder showers in the afternoon.
- The temperature is uniformly high and the annual range of temperature is negligible.
- The maximum temperature on any day is around 30 C while the minimum temperature is around 20 C.
- Tropical evergreen forests with dense canopy cover and large biodiversity are found in this climate.
Q 17 – Explain about tropical wet and dry climate (Aw).
Ans. Tropical Wet and Dry Climate (Aw): Tropical wet and dry climate occurs north and south of Af type climate regions. It borders with dry climate on the western part of the continent and Cf or Cw on the eastern part. Extensive Aw climate is found to the north and south of the Amazon forest in Brazil and adjoining parts.
Q 18 – Explain about Mediterranean Climate
Ans. Mediterranean climate occurs around Mediterranean sea, along the west coast of continents in subtropical latitudes between 30 – 40 latitudes. Central California, Central Chile, along the coast in south eastern and south western Australia are examples of this type of climate. These areas come under the influence of subtropical high in summer and westerly wind in winter.
Features:
- The climate is characterised by hot, dry summer and mild, rainy winter.
- Monthly average temperature in summer is around 25 C and in winter below 10 C.
- The annual precipitation ranges between 35 – 90 cm.
Q 19 – Explain about humid sub tropical climate (Cfa).
Ans. Humid subtropical climate lies on the eastern parts of the continent in subtropical latitudes. In this region the air masses are generally unstable and cause rainfall throughout the year.
They occur in eastern United States of America, southern and eastern China, southern Japan, northeastern Argentina, coastal south Africa and eastern coast of Australia.
Features:
- The annual average of precipitation vary from 75-150 cm.
- Thunderstorms in summer and frontal precipitation in winter are common.
- Mean monthly temperature in summer is around 27 C, and in winter it varies from 5 -12 C.
- The daily range of temperature is small.
Q 20 – In which areas do we find Marine west coast climate? Explain about the features of this climate?
Ans. Marine west coast climate (Cfb) is located poleward from the Mediterranean climate on the west coast of the continents. The main areas are: North western Europe, west coast of North America, north of California, southern Chile, Southeastern Australia and New Zealand.
Features:
- Due to marine influence, the temperature is moderate and in winter, it is warmer than for its latitude.
- The mean temperature in summer months ranges from 15 -20 C and in winter 4 -10 C.
- The annual and daily ranges of temperature are small.
- Precipitation occurs throughout the year. Precipitation varies greatly from 50-250cm.
Q 21 – Explain the major climate categories by Koeppen.
Ans. The first level recognises six major climatic types with each group being designated by a capital letter. These major climate categories have the following broad characteristics:
- Tropical moist climates: These are very warm climates found in the tropics that experience high quantities of precipitation. The primary distinguishing characteristic of these climates is that all months have average temperatures above 18 C (64 F).
- Dry climates: These are climates that experience little precipitation during most of the year. Further, potential losses of water from evaporation and transpiration greatly exceed atmospheric input.
- Moist mid-latitude climates with mild winters: In these climates, summer temperatures are warm to hot and winters are mild. The primary distinguishing characteristic of these climates is that the coldest month has an average temperature between 18 C (64 F) and -3 C (27 F).
- Moist mid-latitude climates with cold winters: In these climates, summer temperatures are warm and winters are cold. The primary distinguishing characteristic of these climates is the average temperature of warmest month exceeds 10 C (50 F), and average temperature of coldest is below -3 C (27 F).
- Polar climates: These climates have very cold winters and summers, with no real summer season. The primary distinguishing characteristic of these climates is the warmest month has an average temperature below 10 C (50 F).
- Highland climates: These are climates that are strongly influenced by the effects of altitude. As a result, the climate of such locations is rather different from places with low elevations at similar latitudes.
Q 22 – Explain the climatic changes that has taken place since ancient times. Also explain its causes.
Ans. The type of climate we experience now might be prevailing over the last 10,000 years with minor and occasionally wide fluctuations. The planet earth has witnessed many variations in climate since the beginning. Geological records show alteration of glacial and inter-glacial periods. The sediment deposits in glacial lakes also reveal the occurrence of warm and cold periods. The rings in the trees provide clues about wet and dry periods. Historical records describe the diversities in climate. All these evidences indicate that change in climate is a natural and continuous process. Archaeological findings show that the Rajasthan desert experienced wet and cool climate around 8,000 B.C. During the Pleistocene epoch, glacial and inter-glacial periods occurred, the last major peak glacial period was about 18,000 years ago. The present inter-glacial period started 10,000 years ago. Variability in climate occurs all the time. The nineties decade of the last century witnessed extreme weather events. The 1990s recorded the warmest temperature of the century and some of the worst floods around the world. Europe witnessed “Little Ice Age” from 1550 to about 1850. From about 1885¬1940 world temperature showed an upward trend. After 1940, the rate of increase in temperature slowed down.
Causes of Climate Change: The causes for climate change can be grouped into astronomical and terrestrial causes.
1. The astronomical causes: These are the changes in solar output associated with sunspot activities. Sunspots are dark and cooler patches on the sun which increase and decrease in a cyclical manner. According to some meteorologists, when the number of sunspots increase, cooler and wetter weather and greater storminess occur. A decrease in sunspot numbers is associated with warm and drier conditions.
2. Volcanism: It is considered as another cause for climate change. Volcanic eruption throws up lots of aerosols into the atmosphere. These aerosols remain in the atmosphere for a considerable period of time reducing the sun’s radiation reaching the Earth’s surface. After the recent Pinatoba and El Cion volcanic eruptions, the average temperature of the earth fell to some extent for some years.
3. Greenhouse gases: The most important anthropogenic effect on the climate is the increasing trend in the concentration of greenhouse gases in the atmosphere which is likely to cause global warming.
Q 23 – Explain about Polar climate (E).
Ans. Polar Climates (E) exist poleward beyond 70 latitude. Polar climates consist of two types:
- Tundra (ET);
- Ice Cap (EF).
1. Tundra Climate (ET): The tundra climate (ET) is so called after the types of vegetation, like low growing mosses, lichens and flowering plants. This is the region of permafrost where the sub soil is permanently frozen. The short growing season and water logging support only low growing plants. During summer, the tundra regions have very long duration of day light.
2. Ice Cap Climate (EF): The ice cap climate (EF) occurs over interior Greenland and Antarctica. Even in summer, the temperature is below freezing point. This area receives very little precipitation. The snow and ice get accumulated and the mounting pressure causes the deformation of the ice sheets and they break. They move as icebergs that float in the Arctic and Antarctic waters. Plateau Station, Antarctica ,79 S, portray this climate.
Q 24 – Explain about Cold snow forest climates (D).
Ans. Cold Snow Forest Climates (D) occur in the large continental area in the northern hemisphere between 40 -70 north latitudes in Europe, Asia and North America. Cold snow forest climates are divided into two types:
- Df- cold climate with humid winter;
- Dw- cold climate with dry winter.
The severity of winter is more pronounced in higher latitudes.
1. Cold climate with humid winters (Df): Cold climate with humid winter occurs poleward of marine west coast climate and mid latitude steppe. The winters are cold and snowy. The frost free season is short. The annual ranges of temperature are large. The weather changes are abrupt and short. Poleward, the winters are more severe.
2.Cold climate with dry winters (Dw): Cold climate with dry winter occurs mainly over Northeastern Asia. The development of pronounced winter anti cyclone and its weakening in summer sets in monsoon like reversal of wind in this region. Poleward summer temperatures are lower and winter temperatures are extremely low with many locations experiencing below freezing point temperatures for up to seven months in a year. Precipitation occurs in summer. The annual precipitation is low from 12-15 cm.
Q 26 – Write a detailed note on Tropical monsoon climate (Am).
Ans. Tropical monsoon climate, occasionally also known as a tropical wet climate or tropical monsoon and trade-wind littoral climatein climate classification, is a relatively rare type of climate that corresponds to the Koppen climate classification category “Am”.
Tropical monsoon climates have monthly mean temperatures above 18 C in every month of the year and feature wet and dry seasons, as Tropical savanna climates do. Unlike tropical savanna climates however, a tropical monsoon climate’s driest month sees less than 60 mm of precipitation but more than (100 [total annual precipitation [mm}/25]). Also, a tropical monsoon climate tends to see less variance in temperatures during the course of the year than a tropical savanna climate. This climate has a driest month which nearly always occurs at or soon after the “winter” solstice for that side of the equator. Tropical monsoon climates are most commonly found in South and Central America. However, there are sections of South Asia, Southeastsia, Africa (particularly West and Central Africa), the Caribbean, and North America that also features this climate.
Q 27 – Explain about that region where there is no permanent settlements for human beings.
Ans. Polar Climates (E) exist poleward beyond 70° latitude. There are no permanent human settlements. Only some scientists live there temporarily for their research and tasks related to manmade satellites.
Polar climates consist of two types:
- Tundra (ET);
- Ice Cap (EF).
1. Tundra Climate (ET): The tundra climate (ET) is so called after the types of vegetation, like low growing mosses, lichens and flowering plants. This is the region of permafrost where the sub soil is permanently frozen. The short growing season and water logging support only low growing plants. During summer, the tundra regions have very long duration of day light.
2. Ice Cap Climate (EF): The ice cap climate (EF) occurs over interior Greenland and Antarctica. Even in summer, the temperature is below freezing point. This area receives very little precipitation. The snow and ice get accumulated and the mounting pressure causes the deformation of the ice sheets and they break. They move as icebergs that float in the Arctic and Antarctic waters. Plateau Station, Antarctica, 79°S, portray this climate.
Q 28 – Give the letter codes used by Koeppen for following types of climates.
- Tropical Wet
- Sub tropical steppe
- Humid Subtropical
- Humid Continental
- Polar Ice cap
- Mid Latitude desert
- Subarctic
- Highlands with snow cover
- Ans. Af
- BSh
- Cfa
- Df
- EF
- BWk
- Dw
- H.
Q 29 – Which letter code did Koeppen use for following temperature ranges?
- Average temperature of the coldest month is 18° or higher.
- Average temperature for all months is below 10° C.
- Average temperature of the coldest month is -3° or lower.
- Average temperature of the coldest month is higher than -3° but less than 18°.
Ans.
- A – Tropical climates
- E – Cold Climates
- D – Cold Snow Forest Climates
- C – Warm Climates.
Q 30 – What is a climatic region?
Ans. A climatic region is defined as an area on the earth’s surface, where an approximately homogenous set of climatic conditions is produced by the combined effect of climatic groups.
Q 31 – Into how many regions was the earth divided by the ancient Greeks?
Ans. The earth was divided into three regions, the winterless tropical region, the summerless polar region, and the intermediate having both 1 winter and summer.
Q 32 – What criteria was followed by KOEPPEN to classify climates?
Ans. KOEPPEN’s classification is based upon annual and monthly r means of temperature and precipitation.
Q 33 – Why did Trewartha use only a limited number of climatic types?
Ans. Because he realized that a large number of climatic types and sub-types are too difficult to remember.
Q 34 – How do human activities add methane and carbon dioxide to the atmosphere?
Ans. Methane and carbon dioxide are added to the atmosphere by burning fossil fuels and by various agricultural activities.
Q 35 – What is the Greenhouse effect on the atmosphere?
Ans. The concept of heating of the atmosphere indirectly from the earth’s surface is called the Greenhouse effect.
Q 36 – Which elements serve as major determinants of climate?
Ans. Climate is long-term meaning daily weather conditions as determined by temperature, precipitation, pressure, winds, and humidity.
Q 37 – Which element is regarded as the basic factor of climate and why?
Ans. Temperature is regarded as the basic factor of climate because other elements are directly or indirectly related to it.’
Q 38 – Name the major divisions of the world on the basis of temperature.
Ans. On the basis of temperature, the world has been divided into three zones, viz., Torrid, Frigid, and Temperate.
Q 39 – Mention various climatic regimes based on rainfall patterns.
Ans. Wet climates, humid climates, sub-humid climates, semi-arid climates, and arid climates are the various regimes based on rainfall patterns.
Q 40 – Name the scholars who have attempted to devise the classification of world climates.
Ans. Vladimir Peter KOEPPEN, C.W. Thomthwaite, and Glen T. Trewartha have so far presented a classification of world climates.
Q 41 – What climatic group is designated by ‘A’ type climate in Trewartha’s classification?
Ans. In Trewartha’s classification, ‘A’ type climate designates ‘Tropical Humid Climate’.
Q 42 – Which type of climate is represented by ‘Ar’?
Ans. Ar’ represents the tropical wet climate.
Q 43 – What is the other name of tropical wet and dry climate?
Ans. The tropical wet and dry climate is also called the ‘Savanna’ climate.
Q 44 – Name two sub-types of polar climate.
Ans. The two sub-types of polar climate are Tundra and Ice-cap.
Q 45 – Name the principal Greenhouse gases.
Ans. Carbon dioxide, methane, and chlorofluorocarbon are the principal gases of the Greenhouse effect.
Q 46 – Which element is common in the principal Greenhouse gases?
Ans. Carbon is the common element in principal Greenhouse gases.
Q 47 – In which part of the world ice-coring program have been undertaken so far?
Ans. So far, the ice-coring programs have been undertaken in Antarctica and Greenland ice-caps.
Q 48 – Name the important elements of climate.
Ans.
- Temperature,
- Precipitation.
Q 49 – Who did the first classification of climate?
Ans. Greeks.
Q 50 – What was the basis of classification done by Greeks?
Ans. Temperature.
Q 51 – Into how many main groups did Trewartha divide the world climate?
Ans. Into six groups.
Q 52 – Which type of climate is known for the minimum range of annual temperature?
Ans. Equatorial climate.
Q 53 – What is the characteristic of the steppe type of climate?
Ans. It is characterized by meager rainfall, low temperature, location in the interiors, and the effects of mountain barriers.
Q 54 – Explain why the tropical humid climate is found in an irregular belt of 20° to 40° latitudes.
Ans. The tropical belt extends across the two tropics, viz., Tropic of Cancer and Tropic of Capricorn in Northern and Southern hemisphere respectively. It is one of the belts which, for part of the year, comes under the influence of trade winds but for the rest of the year is subjected to conventional rain. Moreover, the trade winds which blow from north-east and southeast also bring a considerable amount of rainfall.
Q 55 – What could be the possible consequences of the continued addition of carbon dioxide and methane gases to the atmosphere?
Ans. The continued addition of carbon dioxide and methane gases to the atmosphere will increase the atmospheric temperature to an extent that it will cause ice to melt in the Arctic Ocean and in Antarctica. As a result, sea levels will rise causing the drowning of central lowlands and islands, altering rainfall and evaporation patterns, creating new plant diseases and part problems, and enlarging the ozone hole. Enlargement of the ozone hole, in turn, will cause more and more ultraviolet radiation to reach the earth’s surface, leading to a further rise in temperature of the lower layers of the atmosphere.
Q 56 – Discuss the bases of climatic classifications of Koeppen and Thornth waite
Ans. . Koeppen’s classification is based upon annual and monthly means of temperature and precipitation. Native vegetation was considered as the best expression of the totality of climate. Similarly, Thornthwaite followed Koeppen’s principle that plant is nature’s meteorological instrument capable of integrating climatic elements like precipitation effectiveness and potential evapotranspiration.
Q 57 – Discuss the aims and objectives of Trewartha’s classification.
Ans. Trewartha believed that people who need to understand and use the climatic environment for their own purposes should have the parts of climate presented realistically. At the same time, he also recognized the merits of the genetic type of climatic classification. According to him, “genetic not only increases interest and adds to the scientific quality of climatic analysis, but also gives an extra dimension of insight to the student’s understanding of the description.” Genetic classification of climates emphasizes the causes or origin of their formation based on weather processes.
Q 58 – What type of weather conditions characterizes sub-tropical climate?
Ans. Sub-tropical climates are found between tropical and temperate climatic zones. In this type of climate, the temperature is above 18°C for nearly 8 months. Winters are mild and short. The coastal areas have rainfall throughout the year while continental areas receive less rainfall.
On the basis of seasonal distribution of precipitation, sub-tropical climates have two sub-types, viz., sub-tropical humid and sub-tropical dry summer climates.
Q 59 – How do the carbon dioxide contents of the atmosphere play a dominant role in causing worldwide climatic changes?
Ans. The carbon dioxide contents of the atmosphere play a dominant role in causing worldwide climatic change. Carbon dioxide is transparent to incoming solar radiation but absorbs outgoing longwave terrestrial radiation. The absorbed terrestrial radiation is radiated back to the earth’s surface. Thus, it is clear that any appreciable change in carbon dioxide content would bring about changes in the temperature of the atmosphere
Q 60 – Explain the Greenhouse effect.
Ans. The concept of heating of the atmosphere indirectly from the earth’s surface is called the greenhouse effect. This effect of the atmosphere is analogous to that of a glasshouse, which lets through most of the incoming short wave solar energy but greatly retards the outgoing longwave earth radiation, thus maintaining surface temperatures considerably higher than they otherwise would be. One can build an instantaneous greenhouse. If the car is parked in the sun for about two hours with the windows closed, the interior temperature will rise. It will be more than the temperature outside.
Q 61 – Describe major reservoirs of carbon on earth.
Ans. The carbon in the system moves between several major reservoirs. The atmosphere contains more than 750 billion tonnes of carbon at any given time, while 2000 billion tonnes are stored on land, and approximately 4000 billion tonnes are contained in the ocean. Living terrestrial organic matter is estimated to contain between 450 and 600 billion tonnes. World fossil fuel reserves also constitute an important carbon reservoir of some 5000 billion tonnes. The burning of fossil fuels adds more than 5 billion tonnes of carbon dioxide to the atmosphere every year.
Q 62– Explain why the tropical humid climate is found in an irregular belt of 20° to 40° latitude.
Ans. The tropical belt extends across the two tropics, viz., Tropic of Cancer and Tropic of Capricorn in Northern and Southern hemispheres respectively. It is one of the belts which, for part of the year, comes under the influence of trade winds but for the rest of the year is subjected to convectional rain. Moreover, the trade winds which blow from north-east and south-east also bring a considerable amount of rainfall.
Q 63 – What are ice-coring programs? How do they help us know about the climate of the earth in the past?
Ans. Ice-coring programs analyze the trapped gases in Greenland and Antarctica ice-caps during the last 1,00,000 years. Analysis of these trapped gases, like oxygen, carbon dioxide, etc., reveals the cooling or heating trends of the earth, on the basis of which climatic changes have been studied in the past.
Q 64 – Distinguish between Genetic and Empirical classification of climate?
Ans. Genetic classification of climates emphasizes the cause or origin of their formation based on weather processes. The Empirical classification, on the other hand, is based on observations related to factors for climatic differentiation.
Q 65 – Divide the world into temperature zones.
Ans.The earth is divided into three main temperature zones :
1. Torrid Zone (Hot Zone): Occurs between 0° to 30° N and S latitudes with a mean annual temperature of more than 20°C
2. Temperate Zones: Subdivided into
(a) warm temperate zone (between 10° to 20°C temperature, 30° to 40° N and S),
(b) cool temperate zone (0°C to 10°C temperature, 45° to 60° N and S)
3. Frigid Zones (Cool Zones): Occur between 60° to 90° N and S latitudes.