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Monday 21 August 2017

Gravity's Tug of Pull and Weather.


The rarefying effects of gravitational tug of pull between mountains and continental masses can disperse clouds in certain times of the year, at the center point leaving an area of sunshine. The same effect acting on water or moisture synthetises salt producing brine like in sea water.


Influence Of Gravitational Tug Of Pull Between Mountains On Weather And Climate:

Among the many influences gravity has on weather and climate is by an effect produced at the gravitational center of pull between mountains or continental masses. At this point, a rarefying gravitational field can produce different conditions depending on the period of the year as planets respond to different conditions of gravitational fluctuations. 
In particular times, the mountains pull clouds along with moisture away from the central area leaving a sunny weather condition. 

The rarefying gravitational field has synthesizing effects which produce salt and are partly responsible for the saline in Sea water.
In other times of the year, orbital gravitational fluctuations produces reverse effects where the gravity repels clouds and moisture to the central point. This process produce clouds and rainfall which tend to concentrate on low level ground. Heavy and thick clouds such as cumulonimbus are particularly affected by this characteristic. However, in generalized moisture, the effect may not be evident because of  a cloud cover which make it difficult to tell the thick concentration.
In other times of the year, orbital gravitational fluctuations produce reverse effects in which the gravity of the mountains or continental masses repel clouds to the central point producing a rainfall which concentrate on low level ground.

This effect is produced in distant land masses and not necessarily as shown in the illustrations above. The land masses can be arranged in different ways; in circles, in individual mountains with a common central point of pull or in form of continental masses or high ground.

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