Formations of negative static charges (e⁻) throughout troposphere are natural phenomena revealed by some weather events such as storms and lightning flashes that accompany thunderclouds. These meteorological phenomena (formation of negative charge in that case) have long been considered as events limited in time (i.e., transient process) and space (i.e., isolated process). Now we have good reasons to say that this perception of troposphere electrical status was totally meaningless. Indeed, it is now easy [1] -[4] to show that thunderstorms provide significant numbers of electrons to troposphere at each of their (thunderstorms in this case) appearance. Thereafter, movement implemented in the troposphere by Rossby waves (e.g., West African aerojet) contributes to the formation of low altitudes Electrojets (e.g., West African Equatorial Aerojet gives birth to West African Equatorial Electrojet). Until today, the existence of low layers Equatorial Electrojets (LL-EEJ) was totally ignored by researchers [5] -[22] who use space or ground base data to study Ionosphere’s Equatorial Electrojet (EEJ) and this has led many of them to errors, in their attempt to explain the longitudinal and seasonal variations of observed EEJ. In this paper, we are going to give very useful and unique explanations on the manner in which clouds provide oxygen to troposphere and thereafter trigger negative static charges (e⁻) throughout both troposphere and ionosphere. Indeed, this paper will also explain how, opportunely, the ITF (inter tropical front) plays the role of the tap which provides oxygen to ionosphere: which oxygen thereafter triggers ionospheres’ Equatorial Electrojet (EEJ).

In the past, researchers have often mentioned the presence of condensation nuclei in the atmosphere to trigger the fall of water droplets (solid or liquid) contained in the clouds. This concept (very popular in the 18th century) has not been sufficiently exploited and this led to an erroneous definition of the cloud. In a very recent work [2] , we define the cloud as a gas formed by dry air and saturated water vapor. Misperception of the processes responsible for the formation of clouds has long moved away researchers from the true nature of weather’s processes behind the formation of precipitation. These weather’s processes are closely related to the management of irradiative energy or latent and sensible heat flux (Figure 1).

According to relevant explanations of our study, researchers must next time considered electrons which exist in Troposphere. New and unique description of TEC is now available to make this important correction (Figure 6) and better understand the based and observed EEJ. Taking in account the fact that electrical status of the Troposphere depends mainly on regional variations in the coverage of high clouds and low clouds (Figure 1) and (this is an important remark) on the regional coverage of dioxide Carbon (CO₂) emissions, EEJ longitudinal and seasonal variation will now be clearly explained.

This study opens new research avenues. Moreover, rains provide oxygen and thereafter electrons both to troposphere and ionosphere. Each thunder (or lightning flash) formally highlights the presence of significant numbers of electrons in the troposphere. It is therefore wrong to think that lightning flashes, which are clear evidence of the formation of recombination currents, can completely eliminate all negative charges that have allowed their appearances within the troposphere. New and unique descriptions of TEC are now available and must lead to important corrections and accurate interpretations of the based and observed EEJ. Taking into account the fact that electrical status of the troposphere depends mainly on regional variations in the coverage of high clouds and low clouds (Figure 1) and (this is an important remark) on the regional coverage of dioxide Carbon (CO₂) emissions, EEJ longitudinal and seasonal variations are closely parallel to ITF (Inter Tropical Front) summers’ and winters’ extremes (Figure 7(a), Figure 7(b)).

For their truthful and fruitful interest to space weather sciences, the author wants to acknowledge:

Ÿ Endawoke Yizengaw, Boston College, USA.

Ÿ Patricia Doherty, Boston College, USA.

Ÿ Amory Mazaudier Christine, France.

Ÿ Babatunde Rabiu, Nigeria.

Ÿ Vafi Ndoumbia, Ivory Coast.

Ÿ Obrou Olivier, Ivory Coast.

Cesar MbaneBiouele, (2015) Useful and Unique Descriptions of Tropospheric Processes Which Produce Oxygen and Thereafter Give Birth to Equatorial Electro-Jets. International Journal of Geosciences,06,1248-1253. doi: 10.4236/ijg.2015.611098