4 research outputs found
The Organization of Processes Cycles Forming a Climate and Environment. II. Landscape Transformation and Reorganization of Process Cycles
ΠΡΠΎΠ±Π»Π΅ΠΌΡ ΡΡΠ°Π½ΡΡΠΎΡΠΌΠ°ΡΠΈΠΈ Π»Π°Π½Π΄ΡΠ°ΡΡΠ° ΠΏΠΎΠ΄ Π²ΠΎΠ·Π΄Π΅ΠΉΡΡΠ²ΠΈΠ΅ΠΌ ΡΠΎΡΠ΅ΡΠ°Π½ΠΈΡ ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
,
Π³ΠΈΠ΄ΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈ Π°Π½ΡΡΠΎΠΏΠΎΠ³Π΅Π½Π½ΡΡ
ΡΠ°ΠΊΡΠΎΡΠΎΠ², ΠΏΠ΅ΡΠ΅ΡΡΡΠΎΠΉΠΊΠΈ ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΈ ΡΠΈΠΊΠ»ΠΎΠ²
ΡΡΠ΅Π΄ΠΎΠΎΠ±ΡΠ°Π·ΡΡΡΠΈΡ
ΠΈ ΠΊΠ»ΠΈΠΌΠ°ΡΠΎΠΎΠ±ΡΠ°Π·ΡΡΡΠΈΡ
ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½Ρ Π½Π° ΠΎΡΠ½ΠΎΠ²Π΅ ΡΠΎΠ²ΠΌΠ΅ΡΡΠ½ΠΎΠ³ΠΎ
Π°Π½Π°Π»ΠΈΠ·Π° ΡΠΎΠΏΡΡΠΆΠ΅Π½Π½ΡΡ
ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠΉ ΡΡΠ΅Π΄, ΠΊΠΎΠΌΠΏΠΎΠ½Π΅Π½ΡΠΎΠ² Π³Π΅ΠΎΡΡΠ΅ΡΡ ΠΈ ΠΌΠ΅ΠΆΡΠΈΡΡΠ΅ΠΌΠ½ΡΡ
ΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΠΉ
Π² ΡΠ΅Π³ΠΈΠΎΠ½Π°Π»ΡΠ½ΠΎΠΉ ΠΏΡΠΈΡΠΎΠ΄Π½ΠΎ-ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΎΠΉ ΡΠΈΡΡΠ΅ΠΌΠ΅.
ΠΡΡΠ²Π»Π΅Π½Ρ ΡΠ΅ΠΏΠΈ ΠΏΡΠΈΡΠΈΠ½Π½ΠΎ-ΡΠ»Π΅Π΄ΡΡΠ²Π΅Π½Π½ΡΡ
ΡΠ²ΡΠ·Π΅ΠΉ ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ². ΠΠΏΡΠ΅Π΄Π΅Π»Π΅Π½Ρ ΡΡΠ½ΠΊΡΠΈΠΈ Π²Π»ΠΈΡΠ½ΠΈΡ
ΡΠΎΡΠ΅ΡΠ°Π½ΠΈΠΉ ΡΠ°ΠΊΡΠΎΡΠΎΠ² Π½Π° Π³ΠΈΠ΄ΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΏΡΠΎΡΠ΅ΡΡΡ. Π Π°Π·Π²ΠΈΡΠ° ΠΊΠΎΠ½ΡΠ΅ΠΏΡΠΈΡ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ
ΠΌΠΎΠ΄ΠΈΡΠΈΡΠΈΡΠΎΠ²Π°Π½Π½ΠΎΠ³ΠΎ ΡΠΈΠΊΠ»Π° ΡΡΠ΅Π΄ΠΎΠΎΠ±ΡΠ°Π·ΡΡΡΠΈΡ
ΠΈ ΠΊΠ»ΠΈΠΌΠ°ΡΠΎΠΎΠ±ΡΠ°Π·ΡΡΡΠΈΡ
ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΠΏΡΠΈ
ΡΡΠ°Π½ΡΡΠΎΡΠΌΠ°ΡΠΈΠΈ Π»Π°Π½Π΄ΡΠ°ΡΡΠΎΠ². Π Π°Π·ΡΠ°Π±ΠΎΡΠ°Π½Π° ΡΡΡΡΠΊΡΡΡΠ° ΠΊΠΎΠ½ΡΠ΅ΠΏΡΡΠ°Π»ΡΠ½ΠΎΠΉ ΠΌΠΎΠ΄Π΅Π»ΠΈ ΠΏΠ΅ΡΠ΅ΡΡΡΠΎΠΉΠΊΠΈ
ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΈ ΡΠΈΠΊΠ»Π° ΠΊΠ»ΠΈΠΌΠ°ΡΠΎΠΎΠ±ΡΠ°Π·ΡΡΡΠΈΡ
ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΠΈ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΌΠ΅ΡΡΠ½ΡΡ
ΠΏΡΠΈΡΠΎΠ΄Π½ΠΎ-
ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΡΠ»ΠΎΠ²ΠΈΠΉ. Π‘ΡΠ΅Π΄ΡΡΠ²Π° ΠΎΠΏΠΈΡΠ°Π½ΠΈΡ ΠΏΡΠΈΡΠΎΠ΄Π½ΡΡ
ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΠΈ ΡΠΎΡΠ΅ΡΠ°Π½ΠΈΡ ΡΠ°ΠΊΡΠΎΡΠΎΠ²,
ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΈ ΠΌΠ΅ΠΆΡΠΈΡΡΠ΅ΠΌΠ½ΡΡ
ΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΠΉ ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡΡ ΠΏΡΠΎΠ²ΠΎΠ΄ΠΈΡΡ Π°Π½Π°Π»ΠΈΠ· ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠΉ Π² Ρ
ΠΎΠ΄Π΅
ΡΡΠ°Π½ΡΡΠΎΡΠΌΠ°ΡΠΈΠΈ ΠΊΠΎΠΌΠΏΠΎΠ½Π΅Π½ΡΠΎΠ².Problems of landscape transformation under influence of climatic, hydrological, and anthropogenesis
factors combination and reorganization of the environmental and climate formation cycles have been
investigated. It has been done by means of the joint analysis of the associated changes of environments,
geosphere components and intersystem relations in regional natural and climatic system.
Chains of cause-effect relations of processes are revealed, and influence functions of factor
combinations on the hydrological processes are defined. The formation concept of the modified forming
cycle of environment and climate processes under transformation of landscapes has been developed.
The structure of conceptual model of reorganization of the cycle organization of climate processes and
formation of local natural and environmental conditions has been developed. The means of description
of the natural processes and the factor combination, the organization of interconnections allow the
analysis of changes in the transformation of the components
The Organization of Processes Cycles Forming a Climate and Environment. II. Landscape Transformation and Reorganization of Process Cycles
ΠΡΠΎΠ±Π»Π΅ΠΌΡ ΡΡΠ°Π½ΡΡΠΎΡΠΌΠ°ΡΠΈΠΈ Π»Π°Π½Π΄ΡΠ°ΡΡΠ° ΠΏΠΎΠ΄ Π²ΠΎΠ·Π΄Π΅ΠΉΡΡΠ²ΠΈΠ΅ΠΌ ΡΠΎΡΠ΅ΡΠ°Π½ΠΈΡ ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
,
Π³ΠΈΠ΄ΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈ Π°Π½ΡΡΠΎΠΏΠΎΠ³Π΅Π½Π½ΡΡ
ΡΠ°ΠΊΡΠΎΡΠΎΠ², ΠΏΠ΅ΡΠ΅ΡΡΡΠΎΠΉΠΊΠΈ ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΈ ΡΠΈΠΊΠ»ΠΎΠ²
ΡΡΠ΅Π΄ΠΎΠΎΠ±ΡΠ°Π·ΡΡΡΠΈΡ
ΠΈ ΠΊΠ»ΠΈΠΌΠ°ΡΠΎΠΎΠ±ΡΠ°Π·ΡΡΡΠΈΡ
ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½Ρ Π½Π° ΠΎΡΠ½ΠΎΠ²Π΅ ΡΠΎΠ²ΠΌΠ΅ΡΡΠ½ΠΎΠ³ΠΎ
Π°Π½Π°Π»ΠΈΠ·Π° ΡΠΎΠΏΡΡΠΆΠ΅Π½Π½ΡΡ
ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠΉ ΡΡΠ΅Π΄, ΠΊΠΎΠΌΠΏΠΎΠ½Π΅Π½ΡΠΎΠ² Π³Π΅ΠΎΡΡΠ΅ΡΡ ΠΈ ΠΌΠ΅ΠΆΡΠΈΡΡΠ΅ΠΌΠ½ΡΡ
ΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΠΉ
Π² ΡΠ΅Π³ΠΈΠΎΠ½Π°Π»ΡΠ½ΠΎΠΉ ΠΏΡΠΈΡΠΎΠ΄Π½ΠΎ-ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΎΠΉ ΡΠΈΡΡΠ΅ΠΌΠ΅.
ΠΡΡΠ²Π»Π΅Π½Ρ ΡΠ΅ΠΏΠΈ ΠΏΡΠΈΡΠΈΠ½Π½ΠΎ-ΡΠ»Π΅Π΄ΡΡΠ²Π΅Π½Π½ΡΡ
ΡΠ²ΡΠ·Π΅ΠΉ ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ². ΠΠΏΡΠ΅Π΄Π΅Π»Π΅Π½Ρ ΡΡΠ½ΠΊΡΠΈΠΈ Π²Π»ΠΈΡΠ½ΠΈΡ
ΡΠΎΡΠ΅ΡΠ°Π½ΠΈΠΉ ΡΠ°ΠΊΡΠΎΡΠΎΠ² Π½Π° Π³ΠΈΠ΄ΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΏΡΠΎΡΠ΅ΡΡΡ. Π Π°Π·Π²ΠΈΡΠ° ΠΊΠΎΠ½ΡΠ΅ΠΏΡΠΈΡ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ
ΠΌΠΎΠ΄ΠΈΡΠΈΡΠΈΡΠΎΠ²Π°Π½Π½ΠΎΠ³ΠΎ ΡΠΈΠΊΠ»Π° ΡΡΠ΅Π΄ΠΎΠΎΠ±ΡΠ°Π·ΡΡΡΠΈΡ
ΠΈ ΠΊΠ»ΠΈΠΌΠ°ΡΠΎΠΎΠ±ΡΠ°Π·ΡΡΡΠΈΡ
ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΠΏΡΠΈ
ΡΡΠ°Π½ΡΡΠΎΡΠΌΠ°ΡΠΈΠΈ Π»Π°Π½Π΄ΡΠ°ΡΡΠΎΠ². Π Π°Π·ΡΠ°Π±ΠΎΡΠ°Π½Π° ΡΡΡΡΠΊΡΡΡΠ° ΠΊΠΎΠ½ΡΠ΅ΠΏΡΡΠ°Π»ΡΠ½ΠΎΠΉ ΠΌΠΎΠ΄Π΅Π»ΠΈ ΠΏΠ΅ΡΠ΅ΡΡΡΠΎΠΉΠΊΠΈ
ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΈ ΡΠΈΠΊΠ»Π° ΠΊΠ»ΠΈΠΌΠ°ΡΠΎΠΎΠ±ΡΠ°Π·ΡΡΡΠΈΡ
ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΠΈ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΌΠ΅ΡΡΠ½ΡΡ
ΠΏΡΠΈΡΠΎΠ΄Π½ΠΎ-
ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΡΠ»ΠΎΠ²ΠΈΠΉ. Π‘ΡΠ΅Π΄ΡΡΠ²Π° ΠΎΠΏΠΈΡΠ°Π½ΠΈΡ ΠΏΡΠΈΡΠΎΠ΄Π½ΡΡ
ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΠΈ ΡΠΎΡΠ΅ΡΠ°Π½ΠΈΡ ΡΠ°ΠΊΡΠΎΡΠΎΠ²,
ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΈ ΠΌΠ΅ΠΆΡΠΈΡΡΠ΅ΠΌΠ½ΡΡ
ΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΠΉ ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡΡ ΠΏΡΠΎΠ²ΠΎΠ΄ΠΈΡΡ Π°Π½Π°Π»ΠΈΠ· ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠΉ Π² Ρ
ΠΎΠ΄Π΅
ΡΡΠ°Π½ΡΡΠΎΡΠΌΠ°ΡΠΈΠΈ ΠΊΠΎΠΌΠΏΠΎΠ½Π΅Π½ΡΠΎΠ².Problems of landscape transformation under influence of climatic, hydrological, and anthropogenesis
factors combination and reorganization of the environmental and climate formation cycles have been
investigated. It has been done by means of the joint analysis of the associated changes of environments,
geosphere components and intersystem relations in regional natural and climatic system.
Chains of cause-effect relations of processes are revealed, and influence functions of factor
combinations on the hydrological processes are defined. The formation concept of the modified forming
cycle of environment and climate processes under transformation of landscapes has been developed.
The structure of conceptual model of reorganization of the cycle organization of climate processes and
formation of local natural and environmental conditions has been developed. The means of description
of the natural processes and the factor combination, the organization of interconnections allow the
analysis of changes in the transformation of the components
The Organization of Processes Cycles Forming a Climate and Environment I. Problem statement
ΠΡΠΎΠ±Π»Π΅ΠΌΡ ΡΠΊΠΎΡΠΈΡΡΠ΅ΠΌΠ½ΡΡ
ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠΉ ΠΈ ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΈ ΡΠΈΠΊΠ»Π° ΡΡΠ΅Π΄ΠΎΠΎΠ±ΡΠ°Π·ΡΡΡΠΈΡ
ΠΈ
ΠΊΠ»ΠΈΠΌΠ°ΡΠΎΠΎΠ±ΡΠ°Π·ΡΡΡΠΈΡ
ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½Ρ Π² ΡΠ°ΠΌΠΊΠ°Ρ
ΡΠΈΡΡΠ΅ΠΌΠ½ΠΎ-ΡΠ²ΠΎΠ»ΡΡΠΈΠΎΠ½Π½ΠΎΠΉ ΠΌΠ΅ΡΠΎΠ΄ΠΎΠ»ΠΎΠ³ΠΈΠΈ
Π½Π° ΠΎΡΠ½ΠΎΠ²Π΅ ΡΠΎΠ²ΠΌΠ΅ΡΡΠ½ΠΎΠ³ΠΎ Π°Π½Π°Π»ΠΈΠ·Π° ΡΠΎΠΏΡΡΠΆΠ΅Π½Π½ΡΡ
ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠΉ ΡΡΠ΅Π΄, ΠΊΠΎΠΌΠΏΠΎΠ½Π΅Π½ΡΠΎΠ² Π³Π΅ΠΎΡΡΠ΅ΡΡ ΠΈ
ΠΌΠ΅ΠΆΡΠΈΡΡΠ΅ΠΌΠ½ΡΡ
ΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΠΉ Π² ΡΠ΅Π³ΠΈΠΎΠ½Π°Π»ΡΠ½ΠΎΠΉ ΠΏΡΠΈΡΠΎΠ΄Π½ΠΎ-ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΎΠΉ ΡΠΈΡΡΠ΅ΠΌΠ΅. ΠΡΡΠ²Π»Π΅Π½Π°
ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈ Π·Π½Π°ΡΠΈΠΌΠ°Ρ ΡΠΎΠ»Ρ ΠΏΠΎΠ΄Π²ΠΈΠΆΠ½ΡΡ
ΡΠΈΠΊΠ»ΠΎΠ½ΠΎΠ² ΠΈ ΠΏΠΎΠ»ΡΡΠ΅Π½Ρ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΠ΅ ΠΎΡΠ΅Π½ΠΊΠΈ
ΠΈΡ
Π²ΠΊΠ»Π°Π΄Π° Π² ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠ΅ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊ ΠΊΠ»ΠΈΠΌΠ°ΡΠ° ΠΠ°ΠΏΠ°Π΄Π½ΠΎΠΉ Π‘ΠΈΠ±ΠΈΡΠΈ. Π£ΡΠ»ΠΎΠ²Π½ΠΎ ΠΎΠ±ΡΠ°ΡΠΈΠΌΡΠ΅
ΠΏΡΠ΅ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ ΡΠΊΠΎΡΠΈΡΡΠ΅ΠΌ Π²ΡΠ·ΡΠ²Π°ΡΡ ΠΌΠ΅ΠΆΠ³ΠΎΠ΄ΠΎΠ²ΡΠ΅ ΠΈ ΡΡΠ»ΠΎΠ²Π½ΠΎ ΠΎΠ±ΡΠ°ΡΠΈΠΌΡΠ΅ ΠΌΠ½ΠΎΠ³ΠΎΠ»Π΅ΡΠ½ΠΈΠ΅
ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊ ΡΠ΅Π³ΠΈΠΎΠ½Π°Π»ΡΠ½ΠΎΠ³ΠΎ ΠΊΠ»ΠΈΠΌΠ°ΡΠ°.
ΠΠ°ΠΏΡΠ°Π²Π»Π΅Π½Π½ΠΎΡΡΡ ΠΈ Ρ
Π°ΡΠ°ΠΊΡΠ΅Ρ ΡΠ²ΠΎΠ»ΡΡΠΈΠΎΠ½Π½ΠΎ Π·Π½Π°ΡΠΈΠΌΡΡ
ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠΉ Π±ΠΈΠΎΡΠΈΡΡΠ΅ΠΌ, Π² ΡΠΎΠΌ ΡΠΈΡΠ»Π΅ ΠΈ
Π±ΠΈΠΎΡΠ΅Π½ΠΎΠ·ΠΎΠ², ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΡΡΡΡ ΠΈΡ
ΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΡΠΌΠΈ Π² ΡΠ°ΠΌΠΊΠ°Ρ
ΠΌΠ½ΠΎΠ³ΠΎΡΡΠΎΠ²Π½Π΅Π²ΠΎΠΉ ΠΈΠ΅ΡΠ°ΡΡ
ΠΈΠΈ ΠΏΡΠΈΡΠΎΠ΄Π½ΠΎ-
Ρ
ΠΎΠ·ΡΠΉΡΡΠ²Π΅Π½Π½ΡΡ
ΠΈ Π±ΠΈΠΎΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΠΉ. Π‘ΠΎΠΊΡΠ°ΡΠ΅Π½ΠΈΠ΅ Π±ΠΈΠΎΠΌΠ°ΡΡΡ ΠΈ ΠΏΡΠΎΠ΄ΡΠΊΡΠΈΠ²Π½ΠΎΡΡΠΈ
Π±ΠΈΠΎΡΠ΅Π½ΠΎΠ·ΠΎΠ², ΡΠΌΠ΅Π½ΡΡΠ΅Π½ΠΈΠ΅ Π±ΠΈΠΎΡΠ°Π·Π½ΠΎΠΎΠ±ΡΠ°Π·ΠΈΡ ΡΠ²ΠΈΠ΄Π΅ΡΠ΅Π»ΡΡΡΠ²ΡΡΡ ΠΎ Π½Π°ΡΡΡΠ΅Π½ΠΈΠΈ Π΅ΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΡ
ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΡΠΊΡΡΠ΅Π½ΡΠΈΠ²Π½ΠΎΠ³ΠΎ ΡΠ°Π·Π²ΠΈΡΠΈΡ ΡΠΎΠΎΠ±ΡΠ΅ΡΡΠ² ΠΎΡΠ³Π°Π½ΠΈΠ·ΠΌΠΎΠ² Π² Π±ΠΈΠΎΡΡΠ΅ΡΠ΅.Problems of ecosystem changes and the organization of environment and climate formation cycle are
investigated. It has been made within the limits of system-evolutionary methodology on the basis of the
joint analysis of the associated changes of environments, components of the geosphere and intersystem
relations in the regional natural and climatic system. The climatically significant role of mobile
cyclones is revealed, and quantitative estimations of their contribution to the change of characteristics
of a Western Siberia climate are received. Conditionally reversible transformations of ecosystems
cause interannual and conditionally reversible long-term changes of regional climate characteristics.
The direction and character of evolutionary significant changes of biosystems (including biocenosis)
are defined by their relations within the limits of multilevel hierarchy of natural and economic and
bioclimatic relations. A decrease in the biomass and the biocenosis efficiency, and a reduction of
biodiversity testify that the period of the natural accumulation of the biomass and the energy of living
material in the biosphere and the extensive development of organism communities has ended
The Organization of Processes Cycles Forming a Climate and Environment I. Problem statement
ΠΡΠΎΠ±Π»Π΅ΠΌΡ ΡΠΊΠΎΡΠΈΡΡΠ΅ΠΌΠ½ΡΡ
ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠΉ ΠΈ ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΈ ΡΠΈΠΊΠ»Π° ΡΡΠ΅Π΄ΠΎΠΎΠ±ΡΠ°Π·ΡΡΡΠΈΡ
ΠΈ
ΠΊΠ»ΠΈΠΌΠ°ΡΠΎΠΎΠ±ΡΠ°Π·ΡΡΡΠΈΡ
ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½Ρ Π² ΡΠ°ΠΌΠΊΠ°Ρ
ΡΠΈΡΡΠ΅ΠΌΠ½ΠΎ-ΡΠ²ΠΎΠ»ΡΡΠΈΠΎΠ½Π½ΠΎΠΉ ΠΌΠ΅ΡΠΎΠ΄ΠΎΠ»ΠΎΠ³ΠΈΠΈ
Π½Π° ΠΎΡΠ½ΠΎΠ²Π΅ ΡΠΎΠ²ΠΌΠ΅ΡΡΠ½ΠΎΠ³ΠΎ Π°Π½Π°Π»ΠΈΠ·Π° ΡΠΎΠΏΡΡΠΆΠ΅Π½Π½ΡΡ
ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠΉ ΡΡΠ΅Π΄, ΠΊΠΎΠΌΠΏΠΎΠ½Π΅Π½ΡΠΎΠ² Π³Π΅ΠΎΡΡΠ΅ΡΡ ΠΈ
ΠΌΠ΅ΠΆΡΠΈΡΡΠ΅ΠΌΠ½ΡΡ
ΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΠΉ Π² ΡΠ΅Π³ΠΈΠΎΠ½Π°Π»ΡΠ½ΠΎΠΉ ΠΏΡΠΈΡΠΎΠ΄Π½ΠΎ-ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΎΠΉ ΡΠΈΡΡΠ΅ΠΌΠ΅. ΠΡΡΠ²Π»Π΅Π½Π°
ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈ Π·Π½Π°ΡΠΈΠΌΠ°Ρ ΡΠΎΠ»Ρ ΠΏΠΎΠ΄Π²ΠΈΠΆΠ½ΡΡ
ΡΠΈΠΊΠ»ΠΎΠ½ΠΎΠ² ΠΈ ΠΏΠΎΠ»ΡΡΠ΅Π½Ρ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΠ΅ ΠΎΡΠ΅Π½ΠΊΠΈ
ΠΈΡ
Π²ΠΊΠ»Π°Π΄Π° Π² ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠ΅ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊ ΠΊΠ»ΠΈΠΌΠ°ΡΠ° ΠΠ°ΠΏΠ°Π΄Π½ΠΎΠΉ Π‘ΠΈΠ±ΠΈΡΠΈ. Π£ΡΠ»ΠΎΠ²Π½ΠΎ ΠΎΠ±ΡΠ°ΡΠΈΠΌΡΠ΅
ΠΏΡΠ΅ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ ΡΠΊΠΎΡΠΈΡΡΠ΅ΠΌ Π²ΡΠ·ΡΠ²Π°ΡΡ ΠΌΠ΅ΠΆΠ³ΠΎΠ΄ΠΎΠ²ΡΠ΅ ΠΈ ΡΡΠ»ΠΎΠ²Π½ΠΎ ΠΎΠ±ΡΠ°ΡΠΈΠΌΡΠ΅ ΠΌΠ½ΠΎΠ³ΠΎΠ»Π΅ΡΠ½ΠΈΠ΅
ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊ ΡΠ΅Π³ΠΈΠΎΠ½Π°Π»ΡΠ½ΠΎΠ³ΠΎ ΠΊΠ»ΠΈΠΌΠ°ΡΠ°.
ΠΠ°ΠΏΡΠ°Π²Π»Π΅Π½Π½ΠΎΡΡΡ ΠΈ Ρ
Π°ΡΠ°ΠΊΡΠ΅Ρ ΡΠ²ΠΎΠ»ΡΡΠΈΠΎΠ½Π½ΠΎ Π·Π½Π°ΡΠΈΠΌΡΡ
ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠΉ Π±ΠΈΠΎΡΠΈΡΡΠ΅ΠΌ, Π² ΡΠΎΠΌ ΡΠΈΡΠ»Π΅ ΠΈ
Π±ΠΈΠΎΡΠ΅Π½ΠΎΠ·ΠΎΠ², ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΡΡΡΡ ΠΈΡ
ΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΡΠΌΠΈ Π² ΡΠ°ΠΌΠΊΠ°Ρ
ΠΌΠ½ΠΎΠ³ΠΎΡΡΠΎΠ²Π½Π΅Π²ΠΎΠΉ ΠΈΠ΅ΡΠ°ΡΡ
ΠΈΠΈ ΠΏΡΠΈΡΠΎΠ΄Π½ΠΎ-
Ρ
ΠΎΠ·ΡΠΉΡΡΠ²Π΅Π½Π½ΡΡ
ΠΈ Π±ΠΈΠΎΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΠΉ. Π‘ΠΎΠΊΡΠ°ΡΠ΅Π½ΠΈΠ΅ Π±ΠΈΠΎΠΌΠ°ΡΡΡ ΠΈ ΠΏΡΠΎΠ΄ΡΠΊΡΠΈΠ²Π½ΠΎΡΡΠΈ
Π±ΠΈΠΎΡΠ΅Π½ΠΎΠ·ΠΎΠ², ΡΠΌΠ΅Π½ΡΡΠ΅Π½ΠΈΠ΅ Π±ΠΈΠΎΡΠ°Π·Π½ΠΎΠΎΠ±ΡΠ°Π·ΠΈΡ ΡΠ²ΠΈΠ΄Π΅ΡΠ΅Π»ΡΡΡΠ²ΡΡΡ ΠΎ Π½Π°ΡΡΡΠ΅Π½ΠΈΠΈ Π΅ΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΡ
ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΡΠΊΡΡΠ΅Π½ΡΠΈΠ²Π½ΠΎΠ³ΠΎ ΡΠ°Π·Π²ΠΈΡΠΈΡ ΡΠΎΠΎΠ±ΡΠ΅ΡΡΠ² ΠΎΡΠ³Π°Π½ΠΈΠ·ΠΌΠΎΠ² Π² Π±ΠΈΠΎΡΡΠ΅ΡΠ΅.Problems of ecosystem changes and the organization of environment and climate formation cycle are
investigated. It has been made within the limits of system-evolutionary methodology on the basis of the
joint analysis of the associated changes of environments, components of the geosphere and intersystem
relations in the regional natural and climatic system. The climatically significant role of mobile
cyclones is revealed, and quantitative estimations of their contribution to the change of characteristics
of a Western Siberia climate are received. Conditionally reversible transformations of ecosystems
cause interannual and conditionally reversible long-term changes of regional climate characteristics.
The direction and character of evolutionary significant changes of biosystems (including biocenosis)
are defined by their relations within the limits of multilevel hierarchy of natural and economic and
bioclimatic relations. A decrease in the biomass and the biocenosis efficiency, and a reduction of
biodiversity testify that the period of the natural accumulation of the biomass and the energy of living
material in the biosphere and the extensive development of organism communities has ended