
INSOLATION (2)
Presentation
•
Geography
•
9th Grade
•
Medium
Bhagyashree Majalkar
Used 12+ times
FREE Resource
8 Slides • 7 Questions
1
INSOLATION (2)
2
How is Heat Balance Achieved?
1. Conduction
2. Convection
3. Land breeze and sea breeze
So the earth gets heated more because of the terrestrial radiations rather than insolation.
3
Factor affecting the Distribution of Temperature
4
LATITUDE
Temperature decreases with increase in latitude.
5
ALTITUDE
Temperature of the atmosphere and altitude are inter related. The higher the altitude the lower the temperature.
6
DISTANCE FROM THE SEA
Sea breeze and Land breeze.
7
SLOPE OF THE LAND
8
WIND AND OCEAN CURRENTS
9
Multiple Choice
Currents which flow from higher poles latitudes to lower latitudes in Equatorial regions carry ________ .
Warm water to cooler regions.
Cool water to warmer regions
10
Multiple Choice
Reversal in the vertical distribution of temperature is known as _______.
Normal Lapse rate
Inversion of Temperature
11
Multiple Choice
The landmass gets heated and cooled _____
Fast
Slow
12
Multiple Choice
The height of a place above the mean sea level is known as _____.
Latitude
Altitude
13
Multiple Choice
Decrease of temperature by 1 degree with every 166 m increase in height is known as ______ .
Normal Lapse rate
Inversion of temperature
14
Multiple Choice
The heat radiated by the earth which warms the layers of air above it by direct contact is called _______
Convection
Conduction
15
Multiple Choice
The transfer of heat by circulatory movement is called ______.
Convection
Conduction
INSOLATION (2)
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