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Showing posts with label Climatology. Show all posts
Showing posts with label Climatology. Show all posts

Wednesday, 12 August 2020

August 12, 2020

COMPOSITION OF ATMOSPHERE

ATMOSPHERE
Atmosphere is a blanket of gases and contains huge number of solid and liquid collectively called aerosols surrounding the earth from all sides and forms a protective boundary between the outer space and bio-sphere.
An interesting fact about the atmosphere is that density decreases rapidly with altitude. Nearly 99% of the air lies within 30 km of the earth’s surface.
The atmosphere also shields us from the sun’s ultraviolet radiations which are very harmful for plants and animals. Weather and climate is not possible without the presence of atmosphere. It acts transparent to the sun’s short waves radiation and opaque to the long waves radiation which the earth reflects during night. Thus, it maintains the proper heat balance on the earth. Radio communication is not possible without atmosphere. It also helps in the airways transportation which is consider the fastest means of transportations.

ATMOSPHERIC COMPOSITION
It is also called atmospheric chemistry. The entire atmosphere consists of a mixture of gases. These gases governed by Gas Law. Some of the particles in the atmosphere is the atmospheric single atom-, argon, helium and other are the molecules consisting of atoms of two or more than like- water vapour.
The study of atmosphere included many gases. The study of gases began with the work of element in the 17th century. The first gas a study in detail is CO2. It discovered in 1752. There is only small amount of CO2 in the atmosphere.
Our atmosphere constitutes the main following elements, these are as-
  • Gases
  • Water vapour
  • Dust particles


GASES:- 
The principle gases of our atmosphere are as below;
Nitrogen; Nitrogen constitutes the major portion among the atmospheric gases. It is discovered by Rutherford in 1772 and initial name was Mephietic air.
There are following main characteristics of the nitrogen as under;
This gas accounts 78.08% of the total volume of the atmosphere.
It does not easily enter into chemical union with other elements but it is important constituent of many organic compounds.
Its main function in the atmosphere is to regulate combustion by diluting oxygen.
This gas has no colour, taste and its avoid quick burning.
It extent for over 100 km from the earth surface.
It is very important gas for human and most of the plants and animals as it general proteins which is very essential for their nature growth.
Nitrogen is also important for the industrial and commercial view point also.

Oxygen; Oxygen happen to be the most important gas among the all gases because of its following characteristics;
It is called life giver gas. It is very essential for respiration of human being, animals and plants. No life is possible without oxygen.
When any substance burns O2 is consumed.
It extends up to 120 km in the earth’s atmosphere but its main concentration is found up to 16 km.
It is concentrate in our atmosphere is nearly 20.94%.
This gas was first discovered by Joseph Priestley and its initial name was Dephlogistated air.

Carbon-dioxide; CO2 is the third important gas in our atmosphere.
it is concentrate is nearly 0.03%
it is very important gas for the process of photosynthesis by which the green plants make their own food.
It is meteorologically important also because it is transparent to the incoming solar radiation.
It is keep the air warmer near the ground and along with water vapour is largely responsible for greenhouse effect of the atmosphere.
This gas discovered by Jean.
WATER VAPOUR:-
The visible amount of water in our atmosphere is called water vapour.
The amount of water vapour content of air may vary from 0.02% by volume in a cold dry climate to nearly 4% in the humid tropics.
The most important think about water vapour is that 90% of it lies below 6 km and 50% of it lies below 2 km of the atmosphere.
The main sources of water vapour in our atmosphere are the oceans, rivers, lakes, ponds, transpiration of plants etc.
At the equator and tropics the concentration of water vapour is more but as we move toward the poles its concentration decreases.
Significance of water vapour:-
Water vapour is the source of all clouds and precipitation, like CO2, water vapour plays a significance role in the insolation action of the atmosphere in addition but also a part of the incoming solar radiation. Thus, it is an important control in regulating the energy transfer through the atmosphere.

DUST PARTICLES:-
When air below as winds with sufficient speed. It carried large quantities of particles and keep them suspends in the lower layers of the atmosphere. They are derived from the different sources like smoke, agricultural activities, volcanic activities, mining, meteors, transportation forest fire etc.
Sky looks blue due to presence of dust particles in the atmosphere which scattering the blue light.

Friday, 7 August 2020

August 07, 2020

DEFINITION OF CLIMATOLOGY|| NATURE AND SCOPE OF CLIMATOLOGY ||

WEATHER AND CLIMATE
Before know about climatology it’s necessary to know about weather and climate and differentiate between them, because they play vital role in climatology.
Weather and climate are dynamic features of our physical environment. They affect a wide range of human activities to a greater or lesser degree.
In climatology, Weather refers to the state of atmosphere at any given time denoting the short term variations of atmosphere in term of temperature, pressure, wind, moisture, precipitation and visibility. weather is highly variable. It is constantly changing, sometimes from hour to hour and at other times from day to day.
Climate, on the other hand, is the sum total of the variety of weather conditions of an area or a place. Thus, climate may be defines simply as average weather. The term climate denotes a description of aggregate weather condition.
The World Meteorological Organization has suggested a standard period of 31 years for calculating the climatic average of different weather elements.
According to G.F. Taylor “climate is the integration of weather, and weather is the differentiation of climate. The distinction between weather and climate is, therefore, mainly one of time”

CLIMATOLOGY:-  DEFINITION, NATURE AND SCOPE
Climatology is a branch of science that describe and explain the nature of climate how its differ from place to place. The term climatology originated from the two Greek words , ‘Klima’ + ‘Logos’; Klima means the slope of the Earth whereas Logos refers to a discourse or study.
According to Austin Miller; Climatology is a branch of science which discusses the average condition of the weather.
According to Thornthwaite; broads the scope of climatology , when he suggest that the study of the atmosphere as well as that of the earth’s surface from the core of this discipline. This is so because each and every characteristics of climate is determined by the exchange of heat, moisture, and momentum between the earth’s surface and the atmosphere.

NATURE OF  CLIMATOLOGY 
Climatology tries to study both the nature of climates – local, regional or global – and the natural or human-induced factors that cause climates to change. Climatology considers the past and can help predict future climate change. Sometimes it play role as a Climatology and sometimes as a metrology because we study under this about both weather and Climate.  Moreover there are some of the point, that’s we study in Climatology :
- Identification, demarcation, and distribution of different types of climates. 
- Mode of origin of different types of climates. 
- Causes and processes responsible for climatic variation both horizontally and vertically. 
- Different elements of Weather and climate. 
- Interaction of Weather and climate with human society. 
- Impact of climate on human health and activities including physiological and psychological aspect. 

SCOPE OF CLIMATOLOGY
Generally the scope means subject matter of a discipline. So the subject matters of climatology comprises three basic sub-division of the related to science of climatology-
             
1.PHYSICAL CLIMATOLOGY: This branch of climatology specially to explain the factors responsible for bringing about the temporal ad spatial variation in heat exchange, moisture exchange and air movement. These several observation are climatic elements as Insolation , duration of sunshine, temperature, air pressure, precipitation, winds, cloudiness and fog etc.
Physical climatology is closely related to meteorology which includes not only the physics chemistry and dynamics of atmosphere but also many of its direct effect upon the earth’s surface, the ocean.

2. REGIONAL CLIMATOLOGY: Regional climatology describe the various types of climates. A deals with spatial distribution, regional climatology is the concept of a scale in a regional as well  as spatial pattern.
On the basis of the size and the extent of the climatic region, the world is divided into three major regions;

  • Macro-Climatic Region
  • Meso-Climatic Region
  • Micro-Climatic Region

Macro-climatic region is the largest climatic region in which we study the basic factor of climate such as distribution of continents and oceans. Similarly the meso and micro climate are largely controls by local factors. The meso and micro climates of small areas also required differentiation and explanation as a result of micro-climatology, as a branch of also consider sometimes physical climatology where local climate are closely related to surface condition.

3. APPLIED CLIMATOLOGY: In applied climatology we studies the applications of the climatological knowledge to specific practical problems. It analyses the relationship of climatology to other science.In applied climatology the ,main purpose to find out ways and means to make use of our knowledge of climatic elements for the betterment of human life on the earth.
The available climatological data have a great many applications. Because of the rapidly growing literature of climatology and the experience of persons working in the field of climatology. There has emerged many specialized branch in the field of applied climatology. There are bioclimatology, agro-climatology related to agriculture, medical climatology related to medical, urban climatology are the most important example of the various branches of climatology.

In Short, the term climatology is correctly applied to the study of the following five growing fields-
1. Climatological record
2. Theory of climatology or climate
3. Energy and moisture balance of the earth.
4. Study of climate as the environment of living organism.
5. Study of climate as the direct environment of man.