Monsoons cause wet and dry seasons throughout much of the tropics. Monsoons are most often associated with the Indian Ocean. Monsoons always blow from cold to warm regions. The summer monsoon and the winter monsoon determine the climate for most of India and Southeast Asia.

Heavy rainfall in summer is the defining characteristic of Monsoon climate. Although, The spatial distribution of rainfall is uneven – some regions may receive heavy rains & floods, while the others will have to be contented with meagre rains, droughts & famines.

three

Answer

• Monsoon rains in India mainly occur during four months June, July August and September.
• It goes on decreasing from east to west .
• Most of monsoon rains occur during the season of advancing monsoon around 85% of the total annual rainfall.
• monsoon are pulsating in nature.

India has monsoon type of climate. (ii) Monsoon occurs in alteration of dry and wet spells. The intervening dry spells of monsoon is called ‘Breaks’ in monsoon. (iii) There is variation in intensity, frequency and duration of monsoon.

– The amount of rainfall varies from time to time, often resulting in floods and droughts. Sometimes the rainfall occurs early and at times it is delayed. (c)Rainfall occurs mainly in summer. -A large part of the country receives rainfall mainly in the summer from the South West Monsoon winds.

Explanation:Rainfall is mainly Relief (Orographic). Most of the rainfall is caused due to the obstruction of moisture bearing winds by the mountain ranges. As a result, windward side gets heavy rain while the leeward side gets scanty rain. (b)Rainfall is erratic and unpredictable.

1 Answer. The most important feature of the tropical monsoon type of climate is alternation of Seasons.

Tropical monsoon climates have monthly mean temperatures above 18 °C (64 °F) in every month of the year and a dry season. Tropical monsoon climates is the intermediate climate between the wet Af (or tropical rainforest climate) and the drier Aw (or tropical savanna climate).

1. The Reversal of Winds: The climate of India is characterised by the complete reversal of the wind system with the change of seasons. During the winter season, the winds generally blow from northeast to southwest (land to sea), while in summer season the winds blow from southwest to northeast (sea to land).

(i) These are the most widespread forests in India. (ii) They are also called the monsoon forests and are spread over the region. (iii) They receive rainfall between 70 cm and 200 cm. (iv) Trees shed their leaves for about six to eight weeks in dry summer.

Key Characteristics of Temperate Deciduous “Broadleaf” Forest

• Deciduous forests have a long, warm growing season as one of four distinct seasons.
• There is abundant moisture.
• The soil typically is rich.
• Tree leaves are arranged in strata: canopy, understory, shrub, and ground.

Main characteristics of Tropical deciduous forests:

• These are the most widespread forests in India.
• They are also called the monsoon forests and are spread over the region.
• They receive rainfall between 70 cm and 200 cm.
• Trees shed their leaves for about six to eight weeks in dry summer.

Five features of Tropical Deciduous Forest are: They are also called the monsoon forest. They Spread over the region receiving rainfall between 200 cm and 70 cm. Trees of this forest-type shed their leaves for about 6 to 8 weeks in dry summer.

There are two types of Deciduous Forests: Moist Deciduous Forests – Mixture of Trees and Grasses. Dry Deciduous Forests.

Deciduous forests are home to trees such as oak, birch, beech, aspen, elm and maple. Tropical and subtropical forests also have teak trees, palm trees and bamboo.

Main characteristics of Tropical deciduous forests: These are the most widespread forests in India. They are also called the monsoon forests and are spread over the region. They receive rainfall between 70 cm and 200 cm. Trees shed their leaves for about six to eight weeks in dry summer.

Deciduous forests are home to trees such as oak, birch, beech, aspen, elm and maple. Tropical and subtropical forests also have teak trees, palm trees and bamboo. Plants found in these forests include flowers, ferns, mosses and herbs.

Tropical Deciduous Forests – Temperature and Weather They experience an extremely humid climate (almost 80 to 90 percent) usually throughout the year, the temperature averaging to about 30-degree Celsius.

Tropical Deciduous Forest-Types and Characteristics

• Tropical Deciduous forests also known as monsoon forests are found in the belt along the equator between the tropics of Cancer and Capricorn as well as in the humid subtropics.
• In India Tropical Deciduous Forests are found in Madhya Pradesh, Uttar Pradesh, Bihar, Chhattisgarh, Orissa and parts of Maharastra.

This is simply a list of examples of deciduous trees, there are many more types of deciduous trees.

• Red Maple tree (Acer rubrum)
• Sugar Maple tree (Acer saccharum)
• Silver Maple tree (Acer saccharinum)
• Bigleaf Maple tree (Acer macrophyllum)
• White Oak tree (Quercus alba)
• Black Oak tree (Quercus velutina)

Insects, spiders, slugs, frogs, turtles and salamanders are common. In North America, birds like broad-winged hawks, cardinals, snowy owls, and pileated woodpeckers are found in this biome. Mammals in North American temperate deciduous forests include white-tailed deer, raccoons, opossums, porcupines and red foxes.

The average temperature in temperate deciduous forests is 50°F (10°C). Summers are mild, and average about 70°F (21°C), while winter temperatures are often well below freezing. PLANTS: Trees and plants in deciduous forests have special adaptations to survive in this biome.

What are the different types of forests found in India?

• Tropical Deciduous Forests. These trees have broadleafs.
• Tropical Rain Forests. These are also called equatorial rainforests.
• Montane Forests. This type of forest is found in mountain or hilly areas.
• Tropical Thorn forests.
• Swamp Forests.

Forests cover 1/3 of the earth’s surface and contain an estimated 3 trillion trees. Forests exist in dry, wet, bitterly cold, and swelteringly hot climates.

This is largely because year-round night time temperatures in forests remain higher than open areas due to the mixing down of warm air aloft in forests. In addition, snow-covered open areas reflect sunlight while dark forests absorb sunlight and its warmth.

The forest floor is the lowest layer where it is dark, hot, and damp. Only two percent of sunlight gets through the thick canopy trees and understory plants to reach the forest floor. Large-leafed shrubs and saplings (new trees) grow in the patches of sunlight.