Other
Scientific paper
Apr 2003
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003eaeja......600p&link_type=abstract
EGS - AGU - EUG Joint Assembly, Abstracts from the meeting held in Nice, France, 6 - 11 April 2003, abstract #600
Other
Scientific paper
The atmosphere is a complex dynamic system with many stable and unstable states localized in various land and ocean regions with a lot of feedback loop and diversity of interrelations realized between various atmospheric layers - the troposphere and the middle (10 - 120km) and higher (120 - 1000 km) atmosphere. Space-time changes in the atmosphere are determined by external forcings on the atmoshere on the side of both sun and near-space as well as land and ocean regions. Because of the diversity of processes, occurring in the atmosphere, analysing these processes requires the use of the methods of "science of complexity", which are now being developed. First this requires establishing internal (between subsystems) and external (between a subsystem, the sun and earth) relations characteristic of various subsystems in the atmosphere. Modeling and predicting atmospheric phenomena without taking these relations into account inevitably leads to incorrect conclusions, because, in a strongly nonequilibrium system, such as the atmosphere, even weak actions can radically change the direction of evolution. We present here new experimental findings obtained in field observations in the Arctic, Antarctic and equatorial regions by rocket, satellite, air-borne and ground-based instruments. Conclusion: The atmosphere of the planet Earth is consisting of the corresponding layers each of which is working as multimodal laser system (well known in laser physics) and interacting with other layers of the atmosphere as well as with other qeospheres like the mantle, ionosphere, magnetosphere and with outer space; in a layer there are subsystem of standing waves of which amplitudes have been forcing by solar activity and changing global circulation characteristics, it means that solar activity is forcing climate of Earth: the higher solar activity the higher surface temperature and contra versa. We propose the hypothesis which seems most likely to be correct for any open system: R(3)AS(3)ER(3) - Resonance (1/ usual, 2/ parametric, 3/ stochastic) Amplification Stimulated ( Stochastically and Synergetically) by External Radiation (i..e. by electromagnetic, corpuscular and gravitational).
Chakravarty Sudip
Galkina I.
Gupta Sourendu
Jayaraman Anandhan
Kruchenitsky G.
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