Investigation of the consistency of changes in the wavelet phase characteristics of heliocosmic and climatic variables and changes in the components of the word water balance. Part 2

Abstract

The relevance of research: is due to the need to establish true causes and patterns of changes in the hydrometric characteristics of the global water balance as a whole and its components, natural media on Earth.
 Purpose of research: Establishment of patterns of mutual influences and causes of changes in the components of world water balance on Earth: settlement changes in thermal and water resources on the territory of sushi, clouds on continents, lake levels on continents, the Caspian Sea, Arctic Islands, Greenland and mountain glaciers.
 Objects: Temporary series of heliocosmic and global climatic variables constituting a global water balance.
 Methods of research: the method developed by the author of the calculation of the wavelet phase-frequency and phase-temporal characteristics of the group of the studied time series specified at equal intervals of time, with the calculation of their correlation matrices and the construction of the charts of the variables in two coordinate systems, comparative analysis.
 Results of research: It is shown that in cyclical climate change on land, global water balance as a whole and its components in different relative units and phase orientations, depending on the properties of components of water balance, natural environments, two groups of variables are studying: Helicosmic (Baricenric Sun Movements, Solar activity, long-term solar insolation, greenhouse gases, ozone concentration in the ionosphere, elements of the Earth orbit, geomagnetic field) and global temperature climatic variables caused by changes in the helikosmic factors leading from which is the barycentric movements of the Sun. There is a variability of the water balance depending on their geographic locations on continents. It is shown that the calculated changes in thermal and water resources on the territory of the sushi, changes in clouds and levels of lakes on continents at the observed time intervals is significantly interconnected in the phase-frequency domain, coordinated with changes in the heliocosmic variables leading from which is the barycentric movements of the Sun. It is shown that the change in the level of Lake Rudolf, located in Kenya, occurs in antiphase with changes in other lakes from the phase-frequency domain due to changes in the level of the lake in antiphase with changes in evaporation, evaporation and precipitation the calculated changes in thermal and water resources on land ; Such a phenomenon is observed in changes in Lake Neivasha (Kenya). Data analysis obtained at the East station in Antarctica, bottom sediments of the ocean, in 379.3-1.1 thousand years in the past, graphs of changes in the elements of the Earth orbit, established high consistency of changes in the Caspian level with changes in the angle of inclination, precession and eccentricity of the Earth orbits; In Holocene, agreed with changes in solar activity; coordinated with changes in earthquakes, the speed of rotation of the Earth and the duration of the earth's day, as well as the changes in YMO and the El-Nio phenomenon, with changes in evaporation and precipitation on land in the phase-frequency domain due to the influences of heliocosmic factors. It has been established that changes in the components of the water balance of the Arctic Islands, Greenland and the mountain glaciers are divided into two subgroups; The first includes changes in precipitation and drains, to the second, changes in the resulting and increments of balance sheets. The components of the first subgroup are strongly agreed with the changes in the helixosmic factors, the second, with changes in climatic variables with a negative sign in changes in the balances of the Arctic Islands and Greenland; The second subgroup in the balance of mountain glaciers is strongly agreed with changes in the helicosmic variables with a negative sign in the phase-frequency domain in the observed inter. In changes of phase-temporal characteristics of groups of factors are observed lattice structures of differently and unidirectional changes of variables, characterizing stochastic variability in natural environments.