Thursday 24 May 2012

CBSE X G II FOREST AND WILDLIFE RESOURCES

Class X
Geography
Unit II – Forest and Wildlife Resources
Notes

Black blizzards were giant storms of soil and dust that shook the foundations of the economy of the USA in the 1930s. Watch this short video to get an idea about how indiscriminate destruction of ecosystems can play havoc on the survival of mankind:
www.history.com/videos/black-blizzard#black-blizzard

Lichens: Grey/ green/ yellow plant-like organisms that grow on rocks/ walls/ trees

Lepchas: Aboriginal inhabitants of Sikkim

Biodiversity: The variety of life in a particular habitat or ecosystem

Flora: All the plants of a particular place or time

Fauna: All the animals that live wild in a particular area

Endemic species: Species commonly found in a particular area

NGOs: Legally constituted non-governmental organizations that work for social, economic or cultural causes

Navdanya: An Indian NGO for biodiversity which is a network of seed-keepers and organic producers spread across the country

IUCN: International Union for Conservation of Nature

Examples of normal species: cattle, sal, pine, rodents

Examples of endangered species: black buck, crocodile, Indian wild ass, Indian rhino, lion-tailed macaque, sangai (brow-antlered deer)

Examples of vulnerable species: blue sheep, Asiatic elephant, Gangetic dolphin

Examples of rare species: Himalayan brown bear, wild Asiatic buffalo, desert fox, hornbill

Examples of endemic species: Andaman teal, Nicobar pigeon, Andaman wild pig, mithun (Arunachal Pradesh)

Conservation: Protection of plants, animals and natural resources from the damaging effects of human activity

Categories of forests from the conservation perspective: Reserve forests, protected forests, unclassed forests

States having high percentage of unclassed forests: Gujarat, unclassed forests

Forests are primary producers.

Bassia latifolia is the scientific name of mahua tree.

Anthocephalus cadamba is the scientific name of kadamba tree.

Pinus roxburghii is the scientific name of chir pine tree.

Tamarindus indica is the scientific name of tamarind tree.

Mangifera indica is the scientific name of mango tree.

Quercus spp. is the scientific name of the Himalayan oak tree.

Taxus wallachiana is the scientific name of the Himalayan Yew tree.

Taxol is the chemical extracted from the Himalayan Yew.

Bhairodev Dakav Sanctuary was declared by the people of Alwar district, Rajastan.

Narmada Sagar Project is in Madhya Pradesh.

Buxa Tiger Reserve is in West Bengal.

Sunderbans National Park is in West Bengal.

Corbett National Park is in Uttaranchal.

Bandhavgarh National Park is in Madhya Pradesh.

Sariska Wildlife Sanctuary is in Rajastan.

Manas Tiger Reserve is in Assam.

Periyar Tiger Reserve is in Kerala.

State having the largest area under permanent forests is Madhya Pradesh (75%).

Mundas and Santhals are inhabitants of Chota Nagpur region.

Chipko Movement was organized in Uttaranchal.

Beej Bachao Andolan was organized in Tehri region.

Orissa was the first state to pass a resolution for joint forest management.

The apparent increase in the dense forest cover in India in the last decade of the 20th century was due to plantation by different agencies.

Fisheries are dependent on the maintenance of aquatic biodiversity.

India and Nepal provide habitat to two-thirds of the surviving tiger population in the world.

Teak plantations damaged natural forests in south India.

Chir pine plantations damaged oak and rhododendron forests in the Himalayas.

Mahua and kadamba trees are worshipped by Mundas and Santhals.

Tamarind and mango trees are worshipped by the tribals of Orissa and Bihar.

Enrichment plantation is an ironical term for extensive plantation of a single commercially valuable species eliminating the other species.

In Sariska reserve of Rajastan, people fought against mining.

Himalayan Yew is a medicinal plant found in Himachal Pradesh and Arunachal Pradesh.

Taxol is used in treating cancer.

Reserve forests are the most important forests from the conservation perspective.

Reserve and protected forests are considered permanent forests.


The total number of species in the world is about 1.6 million.

India has about 128,000 species, that is, 8% of the total number of species in the world.

About 81,000 species of fauna and 47,000 species of flora are found in India.

Of the 47,000 species of plants found in India, 15,000 are endemic to the country.

The existence of 10% of India’s flora and 20% of India’s mammals is under threat.

Apart from 1500 plant species, 79 mammals, 44 birds, 15 reptiles and 3 amphibians are endangered in India.

The recent rate of extinction of flora and fauna is 50 – 100 times faster than the natural rate.

India’s forest cover is 637,293 km2, that is, 19.39% of the country’s geographical area. Of this, 11.48% is dense forest, 7.76% is open forest and 0.15% is mangrove forest (according to State of Forest Report 1999).
(To access State of Forest Report 2011, visit http://fsi.org.in/sfr_2011.htm)

Asiatic cheetah can move at speeds up to 112 kmph.

Asiatic cheetah was declared extinct in the year 1952.

Indian Wildlife Protection Act was implemented in the year 1972.

Project Tiger was launched in the year 1973.

Plants are added to the list of protected species in the year 1991.

Joint Forest Management came into existence since 1988.

6 plants were added to the list of protected species in 1991.

During 1951-80, 26,000 km2 of forest was converted into agricultural land.

Since 1951, 5000 km2 of forest was cleared for river valley projects.

Narmada Sagar Project inundates 40,000 hectares of forest.

An average American consumes 40 times more resources than an average Somalian.

Tiger population dwindled from 55,000 to 1827 between 1900 and 1973.

India has 27 tiger reserves covering 37,761 km2.

Area of Bhairodev Dakav Sanctuary is 1200 hectares.

50% of India’s forest area is reserved and 33% is protected.

Activities that damaged forests during the colonial period:
Railways
Industry-oriented agriculture
Commercial and scientific forestry
Mining

Why fuel-fodder collection cannot be regarded as a major cause of depletion of forests:
Because fuel-fodder demand is met by lopping rather than felling trees

Factors that affected India’s biodiversity:
Habitat destruction
Hunting and poaching
Over-exploitation
Pollution and poisoning
Forest fires
Unequal access to resources
Inequitable consumption
Differential sharing of responsibility

The need for conservation:
It preserves ecological diversity.
It preserves life support systems like water, air and soil.
It preserves the genetic diversity of plants and animals for better growth of species and breeding.

Thrust of wildlife protection programme:
Banning hunting and poaching
Giving legal protection to wildlife habitats by establishing national parks and sanctuaries
Restricting trade in wildlife

Threats to tiger population:
Poaching for trade
Shrinking habitat
Depletion of prey base species
Growing human population

Impact of dolomite mining in West Bengal:
It threatens Buxa Tiger Reserve.
It disturbed natural habitat.
It disturbed the migration routes of many species including the great Indian elephant.

Wednesday 23 May 2012

CBSE IX G III CLIMATE

Class IX
Geography
Unit IV – Climate
Notes

Drainage: It refers to the physical features associated with the water bodies, rivers and tributaries in an area.

Climate: Sum total of weather conditions and variations over a large area for a long period of time (more than thirty years)

Weather: State of atmosphere over an area at any point of time

Monsoon: Seasonal reversal in the wind direction during a year

Stilts: Pillars or poles that allow a structure to stand at a height above the ground

Terai: The damp region between the Siwaliks and the Northern Plains.

Ferrel’s Law: The winds in the northern hemisphere get deflected to the right and the winds in the southern hemisphere get deflected to the left.

Coriolis force: An apparent force caused by the earth’s rotation and is responsible for the deflection of winds to the right in the northern hemisphere and to the left in the southern hemisphere

Jet streams: Westerly winds blowing at a speed of 110 kmph (in summer) – 184 kmph (in winter) at an altitude of more than 12,000 m in the troposphere

ITCZ: Inter Tropical Convergence Zone is where the north-east trade winds and the south-east trade winds converge.

SO: Southern Oscillation refers to periodic reversal of pressure conditions between the Pacific Ocean and the Indian Ocean.

ENSO: El Nino Southern Oscillations

The year is divided into seasons on the basis of generalized monthly conditions of atmosphere.

The climate of India is described as the monsoon type.

The word ‘monsoon’ is derived from the Arabic word mausim which means season.

Monsoon climate is found in south Asia and south-east Asia.

Precipitation in the Himalayas is mostly in the form of snowfall.

Temperature contrasts and seasonal contrasts are high in landlocked areas and low in coastal areas.

The annual precipitation in India varies from 400cm in Meghalaya to less than 10 cm in Ladakh and western Rajastan.

Most parts of India receive rainfall between the months June and September.

The rainfall in the Northern Plains decreases from east to west.

Tamilnadu coast gets most of its rainfall during the months of October and November.

Houses in Assam are built on stilts to protect people from snakes, damp soil and floods.

In the Terai region and in Goa and Mangalore in the Konkan coast, houses have sloping roofs because the areas experience heavy rainfall.

Houses in Rajastan have thick walls and flat roofs because the temperature is harsh and rainfall is scanty.

Air temperature decreases from the equator towards the poles.

Hills are cooler in summer because temperature decreases with increase in altitude.

The condition of continentality refers to very hot summers and very cold winters.

The sea exerts a moderating influence on the climate.

India’s climate has the characteristics of tropical as well as sub-tropical climates.

The Tropic of Cancer in India runs from the Rann of Kachch in the west to Mizoram in the east.

The average height of the mountains in the northern part of India is 6000 m.

The maximum altitude of the coastal part of India is 30 m.

The Himalayas prevent the cold winds of Central Asia from entering the Indian subcontinent.

India lies in the region of north-easterly winds.

Winds from the high pressure belt of the northern hemisphere get deflected to the right due to the Coriolis force.

Upper air circulation in India is dominated by a westerly flow.

Sub-tropical westerly jet streams are located between 270N and 300N latitudes.

Tropical easterly jet stream is located around 140N latitude.

Western cyclonic disturbances, experienced in the winter months, are caused by the influence of westerly winds from the Mediterranean region.

Western cyclonic disturbances influence the weather of the north and the north-western regions of India.

Tropical cyclones, caused by easterlies, affect the coastal parts of India.

Tropical cyclones occur during the monsoon and also during the months of October and November.

Monsoons are experienced between 200N and 200S latitudes approximately.

The Ganga Plain is known as the equatorial trough or the monsoon trough during the monsoon season.

Normally the atmospheric pressure in the south Pacific Ocean is higher than the atmospheric pressure in the eastern Indian Ocean.

The intensity of monsoon can be predicted by computing the pressure difference between Tahiti in the Pacific Ocean and Darwin in northern Australia.

Negative pressure difference between Tahiti and Darwin indicate average or late monsoons.

El Nino is a warm ocean current that flows past the coast of Peru (South America) in place of the cold Peruvian current every 2-5 years.

El Nino, which starts flowing at Christmas time, is a Spanish word meaning the child.

The duration of monsoon is 100-120 days from early June to mid-September.

A sudden increase in rainfall at the time of the monsoon’s arrival is known as the burst of the monsoon.

The islands of India receive the very first monsoon.

The islands of India receive the monsoon from the first week of April to the first week of May.

Monsoon arrives at the southern tip of India generally by the first week of June.

After reaching Assam, the mountains cause the monsoons to deflect towards the Ganga Plains.

Delhi receives rain from the Bay of Bengal branch of the monsoon tentatively by 29 June.

Monsoon reaches Himachal Pradesh by mid-July.

Retreat of monsoon begins in the north-western states of India by early September.

The monsoon withdraws completely by early December.

The monsoon withdraws from the islands of India from the first week of December to the first week of January.

Four main seasons can be identified in India.

The cold weather season begins from mid-November and extends till February.

December and January are the coldest months.

Warm days and cold nights characterize the cold weather season in India.

During the cold weather season, the north-east trade winds prevail over the country.

The cold weather season in the northern plains is characterized by cyclonic disturbances from the west.

The winter rainfall in the northern part of India is locally known as mahawat.

The peninsular region does not have a well-defined cold season.

The hot weather season in India is from March to May.

Loo refers to the hot, dry winds that blow over north and north-western India during summer.

Localized thunderstorms in West Bengal are known as Kaal Baisakhi.

Pre-monsoon showers in Kerala and Karnataka are known as mango showers.

The windward side of the Western Ghats receives more than 250 cm of annual rainfall.

Monsoons bring the maximum rainfall to the north-eastern part of the country.

North-east India receives about 400 cm of rainfall annually.

Mawsynram in the Khasi Hills receives the highest average rainfall in the world.

Dry spells occur when the axis of the monsoon trough shifts closer to the Himalayas.

The retreating monsoon season is also known as the transition season.

Tropical cyclones hit the east coast during the retreating monsoon season.

The bulk of the rainfall of the Coromandel Coast is derived from depressions and cyclones.


Elements of climate / weather:
-         Temperature
-         Atmospheric pressure
-         Wind
-         Humidity
-         Precipitation

Climatic variations have given rise to variety in the lives of people in terms of
-         the food they eat
-         the clothes they wear and
-         the kind of houses they live in

Factors that influence the climate of a place:
-         latitude
-         altitude
-         pressure and wind system
-         distance from the sea
-         ocean currents
-         relief features

Factors that influence the climatic conditions of India:
-         pressure and surface winds
-         upper air circulation
-         western cyclonic disturbances
-         tropical cyclones

Most of the world’s deserts are located in the western margins of continents because:
-         the winds in the tropics and the subtropics are easterly, so the precipitation in the west coast is scanty
-         west coasts are washed by cold currents

Important types of jet streams:
-         mid-latitude jet streams
-         sub-tropical jet streams

Difference between trade winds and monsoons:
-         trade winds are steady
-         monsoons are pulsating

The two branches of monsoon:
-         the Arabian Sea branch and
-         the Bay of Bengal branch

Seasons in India:
-         the cold weather season
-         the hot weather season
-         the advancing monsoon season
-         the retreating monsoon season

Areas of scanty rainfall:
-         Gujarat
-         Western Rajastan
-         The interior of the Deccan
-         The eastern part of the Sahyadris
-         Leh in Jammu and Kashmir