Skip to main content

Wave as a sin curve

Before discussing the sin curve, we need to know what sin curve is. Actually, according to the rules of quadrant, when the curve of the sin value is drawn, it is called a sin curve. 
According to the quadrant formula, that is to say in Quadrant-I all value positive, in Quadrant-II only sin value is positive and the others are negative. Quadrant-III only tan positive and the others are negative. Quadrant-IV only cos value positive and the others are negative. 
Now, the sea wave always flows in the curve way according to law of Quadrant. So, we can capture the ocean wave as a sin curve. 
Because, when the crest and the trough of the ocean wave are connected to each other vertically separating them from the average sea level, then a circle will be created. If we divide it into 4 quadrants and calculate every sin value then a curve similar to the sin curve is available. So, wave is called sin curve. That is the intersection of the ocean waves on the average sea bottom, crest and trough adhere to a particular rule that is the quadrant follows the formula. 
We can calculate the angles according to the following formulas-
Y= a . sin ϕ                                             Where,
                                                                      Y= Function,
                                                                       a=Amplitude,
                                                                       ϕ=Angle.
Now the amplitude of the 0° angle will be-
Y=a .sin ϕ
   =a . 0
   = 0
Now the amplitude of the 90° angle will be-
Y=a .sin ϕ
   =a.sin90
  = a.1      ₒ°ₒ Amplitude= +1
Now the amplitude of the 180° angle will be-
Y=a .sin ϕ
   =a.sin180°
   =a.sin(2×90°+0)
  =a.sin0°
  0
                                                  So, the wave always flows according to the rules of quadrant. Wave is also called cos curve by many others.
Fig: Wave as a sin curve


Comments

Popular posts from this blog

Behaviouralism in geography

Behaviouralism Behaviouralism is an approach in human geography that came to prominence in the human geography of the 1960s and 1970s. It goes out of the idea that people are the determining factor in the explanation of space. Behaviouralism tries to give an explanation of the spatiallity of human activities. And thereby they use a complex universally applicable model.  Definition of Behaviouralism: The particular aspect with which geographical content is analyzed using mathematical statistics & human sensitivity, is called behavioralism. Concept of Behaviouralism: The Behaviouralism revolution is a theoretical concept. Its theories are not based on assumptions, but are actually explored through ascending methods based on the experience of human behavior. An analysis of the significance of geographical issues in behavioral perspectives within a system, so therefore is no definite boundary to behavioral geography. The main purpose of behaviouralism geography is to in...

Concentric zone theory

Theories of City Structure-Concentric Zone Theory Introduction: The Concentric or Zonal Theory of urban landuse was first proposed in 1923 by E.W. Burgess. He was a sociologist. The idea behind the concentric model is that the development of a city takes place outwards from its central area in a series of concentric circles to form zones.  Assumption:        i.           Cultural & social heterogeneity of the population.       ii.           Commercial-industrial base to the economy of the city.     iii.           Private ownership of property & economic competition for space.     iv.           Expanding area & population of the city.       v.    ...

T-S Diagram

Definition: The diagram by which the salinity & temperature of the sea water are expressed is called T-S diagram. Prepared: T-S Diagram was prepared by Helland Harsenin (1916) with the objective to  determine the density of water at various depth. Characteristics: The Temperature ‘T’ & Salinity ‘S’ observed at the particular depth are represented by a single point in this diagram. The plotted points of T & S generally fall on a well defined curve, in which temperature & salinity decrease together. The density of water tends to increase with depth. In T-S Diagram, it may be observed that many combinations of temperature & salinity can yield the same density. In T-S Diagram, it may be observed that the density of water tends to increase with depth.  Diagrammatic Example: Significance: The T-S Diagram is a tool of great utility in Oceanography. The T-S Diagram is the way to visualize layering of water. The T-S Diagram helps in t...