Access over 20 million homework & study documents

213669263_study_of_the_theory_of_turbulence.doc

Content type
User Generated
Rating
Showing Page:
1/10
Indian Science Cruiser Vol. 27, No. 3, May 2013
Study of the Theory of Turbulence
N.C. Ghosh
Department of Mathematics
Rabindra Bharati University
56A B.T. Road
Kolkata - 50
Email : ncgsnbmms@hotmail.com
Big whirls have little whirls that feed on their velocity:
little whirls have lesser whirls, and so on to viscosity.
Thus E.G. Rechardson expressed the energy cascading principle in turbulence. Perhaps considering
complexities of analysing turbulence one scientist wrote: If there is a god and I can meet him, I will ask him
something about willy-lilly behaviours of turbulent phenomena.
Turbulence is one of the oldest and most difficult open problems in physics. Applied Mathematicians
deals it very carefully from the mathematical stand point of view.
The story is told of many giants of modern physics, but most plausibly of Heisenberg, on his death-
bed, he remarked that the two great unsolved problems were reconciling quantum mechanics and general relativity,
and turbulence. "Now, I'm optimistic about gravity..."
Knowledge of the study of Theory Turbulence is essential


           
 

Knowledge of the study of Theory Turbulence is essential for analyzing many real life situation viz,
For analyzing atmospheric aspects
Continuously moving air in the atmospheric region is a burning example of turbulence. With out the
knowledge of turbulent characteristics of air no way can say a single word perfectly regarding the atmospheric
region.
For Weather forecasting
!          
"#$%&"'"
  (       ) '
#*&&"'+
,*&&&"'-
        
./ (          
/#.
+)
1

Sign up to view the full document!

lock_open Sign Up
Showing Page:
2/10
          /  
 /         
#0
0!1

2
1#/3

4#5
          ( 

,66
7/8

3

For understanding aspects of Cyclone :
Cyclone is a storm accompanied by high speed whistling and howling winds. In meteorology, a
cyclone is an area of low atmospheric pressure characterized by inward spiraling winds that rotate counter
clockwise in the northern hemisphere and clockwise in the southern hemisphere of the Earth. Since the generic
term covers a wide variety of meteorological phenomena, such as tropical cyclones, extratropical cyclones, and
tornadoes, meteorologists rarely use it without additional qualification.
Cold-core cyclones (most cyclone varieties) form due to the nearby presence of an upper level trough,
which increases divergence aloft over an area that induces upward motion and surface low pressure. Warm-core
cyclones (such as tropical cyclones and many mesocyclones) can have their initial start due to a nearby upper
trough, but after formation of the initial disturbance, depend upon a storm-relative upper level high to maintain or
increase their strength.
It is often difficult to predict where a cyclone will strike. When it starts moving from oceans towards the
land area, a cyclone can change track and hit areas other than those anticipated earlier.
To analyse turbulent condition of fluid during Tsunami
(  9 66:       

  ,#       
           
#
  # 6       
#36
6
'  1   
;&
;%&(;&&
#
(6
(6
2

Sign up to view the full document!

lock_open Sign Up
Showing Page:
3/10

Sign up to view the full document!

lock_open Sign Up
End of Preview - Want to read all 10 pages?
Access Now
Unformatted Attachment Preview
Indian Science Cruiser Vol. 27, No. 3, May 2013 Study of the Theory of Turbulence N.C. Ghosh Department of Mathematics Rabindra Bharati University 56A B.T. Road Kolkata - 50 Email?: ncgsnbmms@hotmail.com Big whirls have little whirls that feed on their velocity: little whirls have lesser whirls, and so on to viscosity. Thus E.G. Rechardson expressed the energy cascading principle in turbulence. Perhaps considering complexities of analysing turbulence one scientist wrote: If there is a god and I can meet him, I will ask him something about willy-lilly behaviours of turbulent phenomena. Turbulence is one of the oldest and most difficult open problems in physics. Applied Mathematicians deals it very carefully from the mathematical stand point of view. The story is told of many giants of modern physics, but most plausibly of Heisenberg, on his death-bed, he remarked that the two great unsolved problems were reconciling quantum mechanics and general relativity, and turbulence. "Now, I'm optimistic about gravity..." Knowledge of the study of Theory Turbulence is essential Turbulence is a notoriously difficult subject. The goal is for investigation of such complex phenomena is to debate with some fundamental questions related to this that are wide ranging, from the initiation of turbulence through to its asymptotic state at high Reynolds number, including the effects of rotation and ...
Purchase document to see full attachment
User generated content is uploaded by users for the purposes of learning and should be used following Studypool's honor code & terms of service.

Anonymous
I use Studypool every time I need help studying, and it never disappoints.

Studypool
4.7
Trustpilot
4.5
Sitejabber
4.4