It is also evident that log pCO2 values linearly decreases with pH indicating fresh water recharge or less atmospheric interaction with the system (Chidambaram et al. 2013).
The proposed methodology opens the possibility to assess atmospheric interaction characteristics by using the unprecedented opportunity arising from the numerous observed orbital decay of nanosatellites.
Nanosatellites have gained considerable presence in low Earth orbits wherein the atmospheric interaction with exposed surfaces plays a fundamental role in the evolution of motion.
These different reports could be due to the types of GCM used to generate future rainfall trend (Sarr 2012), differences in topography, temperature, altitude, vegetation cover, atmospheric interaction, and land use management.
On the other hand, their limitation in representing real atmospheric interaction between large scale structures and thermal stratification with the flow pattern can introduce significant errors in evaluating wind energy potential.
Water with high pCO2 of around −1.5 results due to deep circulation of groundwaters, with lesser atmospheric interaction or due to higher saturation of carbonates, resulting from the interaction with the host rock of the material through which it flows (Chidambaram et al. 2011).
