9 research outputs found
A Modified Algorithm for Estimating the Radial Cell Size in the Vaganov-Shashkin Simulation Model
ΠΠΎΠ½ΠΈΠΌΠ°Π½ΠΈΠ΅ ΠΌΠ΅Ρ
Π°Π½ΠΈΠ·ΠΌΠ° ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΈ ΡΠΎΡΡΠ° Π³ΠΎΠ΄ΠΈΡΠ½ΡΡ
ΠΊΠΎΠ»Π΅Ρ Π΄ΡΠ΅Π²Π΅ΡΠ½ΡΡ
ΡΠ°ΡΡΠ΅Π½ΠΈΠΉ ΠΏΠΎΠ΄
Π²Π»ΠΈΡΠ½ΠΈΠ΅ΠΌ Π²Π΅Π΄ΡΡΠΈΡ
ΡΠ°ΠΊΡΠΎΡΠΎΠ² Π²Π½Π΅ΡΠ½Π΅ΠΉ ΡΡΠ΅Π΄Ρ ΡΠ²Π»ΡΠ΅ΡΡΡ ΠΎΠ΄Π½ΠΎΠΉ ΠΈΠ· ΡΠ°ΠΌΡΡ
Π°ΠΊΡΡΠ°Π»ΡΠ½ΡΡ
ΠΏΡΠΎΠ±Π»Π΅ΠΌ
ΡΠΎΠ²ΡΠ΅ΠΌΠ΅Π½Π½ΠΎΠΉ Π΄Π΅Π½Π΄ΡΠΎΡΠΊΠΎΠ»ΠΎΠ³ΠΈΠΈ. Π£ΡΠΊΠΎΡΠ΅Π½ΠΈΠ΅ ΠΈΠ»ΠΈ Π·Π°ΠΌΠ΅Π΄Π»Π΅Π½ΠΈΠ΅ ΡΠΊΠΎΡΠΎΡΡΠΈ ΡΠΎΡΡΠ° Π΄Π΅ΡΠ΅Π²Π° Π² ΠΎΡΠ΄Π΅Π»ΡΠ½ΡΠ΅
ΠΈΠ½ΡΠ΅ΡΠ²Π°Π»Ρ ΡΠ΅Π·ΠΎΠ½Π° ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΠ΅ΡΡΡ ΡΠΎΠ²ΠΌΠ΅ΡΡΠ½ΡΠΌ Π²Π»ΠΈΡΠ½ΠΈΠ΅ΠΌ ΡΠ°ΠΊΠΈΡ
ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΠ°ΠΊΡΠΎΡΠΎΠ²,
ΠΊΠ°ΠΊ ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΠ° ΠΈ Π²Π»Π°ΠΆΠ½ΠΎΡΡΡ ΠΏΠΎΡΠ²Ρ. Π‘ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ΠΌ ΠΌΠΎΠ΄ΠΈΡΠΈΡΠΈΡΠΎΠ²Π°Π½Π½ΠΎΠ³ΠΎ Π°Π»Π³ΠΎΡΠΈΡΠΌΠ°
ΠΈΠΌΠΈΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠΉ ΠΌΠΎΠ΄Π΅Π»ΠΈ ΡΠΎΡΡΠ° Π΄ΡΠ΅Π²Π΅ΡΠ½ΡΡ
ΡΠ°ΡΡΠ΅Π½ΠΈΠΉ ΠΠ°Π³Π°Π½ΠΎΠ²Π°-Π¨Π°ΡΠΊΠΈΠ½Π° β VS-ΠΎΡΡΠΈΠ»Π»ΠΎΠ³ΡΠ°ΡΠ° β
Π² ΡΠ°Π±ΠΎΡΠ΅ ΠΌΠΎΠ΄Π΅Π»ΠΈΡΡΠ΅ΡΡΡ ΡΠ΅Π·ΠΎΠ½Π½ΡΠΉ ΡΠΎΡΡ ΠΊΠ»Π΅ΡΠΎΠΊ Π² Π³ΠΎΠ΄ΠΈΡΠ½ΠΎΠΌ ΠΊΠΎΠ»ΡΡΠ΅. ΠΡΠ΅Π΄Π»ΠΎΠΆΠ΅Π½ Π½ΠΎΠ²ΡΠΉ
ΠΌΠ°ΡΠ΅ΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΠΉ ΠΏΠΎΠ΄Ρ
ΠΎΠ΄ ΠΊ ΠΎΡΠ΅Π½ΠΊΠ΅ ΠΊΠ°ΠΌΠ±ΠΈΠ°Π»ΡΠ½ΠΎΠΉ Π°ΠΊΡΠΈΠ²Π½ΠΎΡΡΠΈ Ρ
Π²ΠΎΠΉΠ½ΡΡ
ΠΈ ΡΠ΅Π·ΠΎΠ½Π½ΠΎΠΉ ΠΊΠ»Π΅ΡΠΎΡΠ½ΠΎΠΉ
ΠΏΡΠΎΠ΄ΡΠΊΡΠΈΠΈ, ΠΊΠΎΡΠΎΡΡΠΉ Π±ΡΠ» ΠΏΡΠΎΡΠ΅ΡΡΠΈΡΠΎΠ²Π°Π½ Π½Π° ΠΎΠ±ΡΠ°Π·ΡΠ΅ ΡΠΎΡΠ½Ρ ΠΎΠ±ΡΠΊΠ½ΠΎΠ²Π΅Π½Π½ΠΎΠΉ (Pinus sylvestris L.),
ΠΎΡΠΎΠ±ΡΠ°Π½Π½ΠΎΠΌ Π² Π₯Π°ΠΊΠ°ΡΠΈΠΈ, Π·Π° ΠΏΠ΅ΡΠΈΠΎΠ΄ Ρ 1969 ΠΏΠΎ 2008 Π³Π³. ΠΠ»Π°Π³ΠΎΠ΄Π°ΡΡ Π΄Π°Π½Π½ΠΎΠΌΡ ΠΏΠΎΠ΄Ρ
ΠΎΠ΄Ρ ΡΠ΄Π°Π»ΠΎΡΡ
ΡΠ°Π·Π΄Π΅Π»ΠΈΡΡ Π²Π»ΠΈΡΠ½ΠΈΠ΅ ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈ Π½Π΅ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
Π²Π½Π΅ΡΠ½ΠΈΡ
ΡΠ°ΠΊΡΠΎΡΠΎΠ² Π½Π° ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅
ΠΊΠ»Π΅ΡΠΎΠΊ Π² Π³ΠΎΠ΄ΠΈΡΠ½ΠΎΠΌ ΠΊΠΎΠ»ΡΡΠ΅ Π΄ΡΠ΅Π²Π΅ΡΠ½ΡΡ
ΡΠ°ΡΡΠ΅Π½ΠΈΠΉTo describe the mechanism of tree-ring formation in woody plants influencing by the leading
environmental factors is one of the most urgent problems of modern dendroecology. Changing of
the tree-ring growth rate at selected intervals in the growing season is determined by the complex
influence of climatic factors (e.g. temperature and soil moisture). Using the modified algorithm of the
simulation model of growth Vaganov-Shashkin β VS-oscilloscope seasonal growth of cells in tree ring
is simulated in the work. New mathematical approach is developed to estimate a cambial activity
and seasonal cell production of conifer species. The approach is tested on tree-ring sample of Pinus
sylvestris for Khakassian region over 1969-2008. The obtained approach allows to separate a treering
growth signal on two components caused by climatic and non-climatic factor
Visual Parameterization of Vaganov-Shashkin Simulation Model and its Application in Dendroecological Research
Π Π΄Π΅Π½Π΄ΡΠΎΡ
ΡΠΎΠ½ΠΎΠ»ΠΎΠ³ΠΈΠΈ ΠΈΡΠΏΠΎΠ»ΡΠ·ΡΠ΅ΡΡΡ Π±ΠΎΠ»ΡΡΠΎΠ΅ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²ΠΎ ΡΠ°Π·Π»ΠΈΡΠ½ΡΡ
Π°Π½Π°Π»ΠΈΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΏΠΎΠ΄Ρ
ΠΎΠ΄ΠΎΠ²
Π΄Π»Ρ Π°Π½Π°Π»ΠΈΠ·Π° Π΄Π°Π½Π½ΡΡ
, ΠΎΠ΄Π½ΠΈΠΌ ΠΈΠ· ΠΊΠΎΡΠΎΡΡΡ
ΡΠ²Π»ΡΠ΅ΡΡΡ ΠΌΠΎΠ΄Π΅Π»ΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅. ΠΡΠΈ ΡΠΎΠ·Π΄Π°Π½ΠΈΠΈ Π»ΡΠ±ΠΎΠΉ ΠΌΠΎΠ΄Π΅Π»ΠΈ
ΠΎΠ΄Π½ΠΈΠΌ ΠΈΠ· Π³Π»Π°Π²Π½ΡΡ
Π²ΠΎΠΏΡΠΎΡΠΎΠ² Π²ΡΡΡΡΠΏΠ°Π΅Ρ Π²ΡΠ±ΠΎΡ Π³Π»Π°Π²Π½ΡΡ
ΡΠ°ΠΊΡΠΎΡΠΎΠ². Π‘Π°ΠΌΡΠ΅ ΡΠ°ΡΠΏΡΠΎΡΡΡΠ°Π½Π΅Π½Π½ΡΠ΅ ΠΈ
Π΄ΠΎΡΡΡΠΏΠ½ΡΠ΅ ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ Π΄Π°Π½Π½ΡΠ΅ β ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΠ° ΠΈ ΠΎΡΠ°Π΄ΠΊΠΈ.
ΠΠ° ΠΎΡΠ½ΠΎΠ²Π°Π½ΠΈΠΈ ΠΈΠΌΠΈΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠΉ ΠΌΠΎΠ΄Π΅Π»ΠΈ ΠΠ°Π³Π°Π½ΠΎΠ²Π°-Π¨Π°ΡΠΊΠΈΠ½Π° ΠΏΡΠ΅Π΄Π»ΠΎΠΆΠ΅Π½ Π½ΠΎΠ²ΡΠΉ Π°Π»Π³ΠΎΡΠΈΡΠΌ
Π²ΠΈΠ·ΡΠ°Π»ΡΠ½ΠΎΠΉ ΠΏΠ°ΡΠ°ΠΌΠ΅ΡΡΠΈΠ·Π°ΡΠΈΠΈ ΡΠΎΡΡΠ° Π³ΠΎΠ΄ΠΈΡΠ½ΡΡ
ΠΊΠΎΠ»Π΅Ρ Ρ
Π²ΠΎΠΉΠ½ΡΡ
Π΄Π΅ΡΠ΅Π²ΡΠ΅Π², Π½Π°Π·Π²Π°Π½Π½ΡΠΉ Β«VS-
ΠΎΡΡΠΈΠ»Π»ΠΎΠ³ΡΠ°ΡΒ», ΠΈ ΠΎΠΏΠΈΡΠ°Π½Π° Π΅Π³ΠΎ ΠΏΡΠΎΠ³ΡΠ°ΠΌΠΌΠ½Π°Ρ ΡΠ΅Π°Π»ΠΈΠ·Π°ΡΠΈΡ. ΠΠΎΠ»ΡΡΠ΅Π½Π½ΡΠΉ Π°Π»Π³ΠΎΡΠΈΡΠΌ Π±ΡΠ»
Π°ΠΏΡΠΎΠ±ΠΈΡΠΎΠ²Π°Π½ Π½Π° Π΄Π²ΡΡ
ΠΏΠΎΡΠΎΠ΄Π°Ρ
Π΄ΡΠ΅Π²Π΅ΡΠ½ΡΡ
ΡΠ°ΡΡΠ΅Π½ΠΈΠΉ β Larix gmelini ΠΈ Picea obovata. ΠΠΎΠ²ΡΠΉ ΡΠΏΠΎΡΠΎΠ±
ΠΏΠ°ΡΠ°ΠΌΠ΅ΡΡΠΈΠ·Π°ΡΠΈΠΈ ΠΈ Π°Π½Π°Π»ΠΈΠ· ΠΌΠΎΠ΄Π΅Π»ΠΈΡΡΠ΅ΠΌΡΡ
ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΠΎΠ² ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡΡ ΠΎΡΠ΅Π½ΠΈΡΡ Π»ΠΎΠΊΠ°Π»ΡΠ½ΡΠ΅ ΡΡΠ»ΠΎΠ²ΠΈΡ
ΠΏΡΠΎΠΈΠ·ΡΠ°ΡΡΠ°Π½ΠΈΡ Π΄ΡΠ΅Π²Π΅ΡΠ½ΡΡ
ΡΠ°ΡΡΠ΅Π½ΠΈΠΉ Π½Π° ΠΎΡΠ½ΠΎΠ²Π΅ Π΄ΠΈΠ½Π°ΠΌΠΈΠΊΠΈ Π΄Π²ΡΡ
ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΏΠ΅ΡΠ΅ΠΌΠ΅Π½Π½ΡΡ
:
ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΡ ΠΈ ΠΎΡΠ°Π΄ΠΊΠΎΠ², Π±Π΅Π· ΠΏΡΠΈΠ²Π»Π΅ΡΠ΅Π½ΠΈΡ Π΄ΠΎΠΏΠΎΠ»Π½ΠΈΡΠ΅Π»ΡΠ½ΠΎΠΉ ΠΈΠ½ΡΠΎΡΠΌΠ°ΡΠΈΠΈ ΠΎ ΠΌΠ΅ΡΡΠΎΠΎΠ±ΠΈΡΠ°Π½ΠΈΠΈThere are many different methods and tools for data analysis in dendrochronology. Modeling is one of
them. One of the main issues in modeling is a choice of the main factors. Π‘limatic data (temperature
and precipitation) are the most common and affordable of them. Based on Vaganov β Shaskin model
the new algorithm of visual parameterization of three-ring growth β VS-oscilloscope was developed.
Algorithm was tested on different species of woody plants β Larix gmelini and Picea obovata. A new
parameterization and analysis of modeling results help to evaluate conditions of area of growth of
woody plants, based on dynamic of two climate variables: temperature and precipitation, without
adding information about area of growt
DYNAMICS OF THE SOIL CO2 EMISSION DURING SNOW-FREE PERIOD IN THE IN MIDDLE TAIGA FORESTS IN CENTRAL SIBERIA
Π’Π΅ΠΊΡΡ ΡΡΠ°ΡΡΠΈ Π½Π΅ ΠΏΡΠ±Π»ΠΈΠΊΡΠ΅ΡΡΡ Π² ΠΎΡΠΊΡΡΡΠΎΠΌ Π΄ΠΎΡΡΡΠΏΠ΅ Π² ΡΠΎΠΎΡΠ²Π΅ΡΡΡΠ²ΠΈΠΈ Ρ ΠΏΠΎΠ»ΠΈΡΠΈΠΊΠΎΠΉ ΠΆΡΡΠ½Π°Π»Π°.ΠΠΎΡΠ²Π° ΡΠ²Π»ΡΠ΅ΡΡΡ ΠΎΡΠ½ΠΎΠ²Π½ΡΠΌ ΡΠ΅Π·Π΅ΡΠ²ΡΠ°ΡΠΎΠΌ ΡΠ³Π»Π΅ΡΠΎΠ΄Π° (C) Π² Π±ΠΈΠΎΡΡΠ΅ΡΠ΅, ΠΈ Π² Π³Π»ΠΎΠ±Π°Π»ΡΠ½ΠΎΠΌ ΠΌΠ°ΡΡΡΠ°Π±Π΅ ΡΠΎΠ΄Π΅ΡΠΆΠΈΡ Π² Π΄Π²Π° ΡΠ°Π·Π° Π±ΠΎΠ»ΡΡΠ΅ C, ΡΠ΅ΠΌ Π°ΡΠΌΠΎΡΡΠ΅ΡΠ°, ΠΈ Π² ΡΡΠΈ ΡΠ°Π·Π° Π±ΠΎΠ»ΡΡΠ΅, ΡΠ΅ΠΌ ΡΠ°ΡΡΠΈΡΠ΅Π»ΡΠ½ΠΎΡΡΡ. ΠΠΎΡΠΎΠΊΠΈ CO2 ΠΈΠ· ΠΏΠΎΡΠ²Ρ ΠΎΡΠ΅Π½Ρ ΡΡΠ²ΡΡΠ²ΠΈΡΠ΅Π»ΡΠ½Ρ ΠΊ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡΠΌ ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΡ, ΠΈ ΠΎΡΠ½ΠΎΡΠΈΡΠ΅Π»ΡΠ½ΠΎ Π½Π΅Π±ΠΎΠ»ΡΡΠΈΠ΅ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡ Π² Π½Π΅ΠΉ ΠΌΠΎΠ³ΡΡ ΠΎΠΊΠ°Π·Π°ΡΡ ΡΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΠΎΠ΅ Π²Π»ΠΈΡΠ½ΠΈΠ΅ Π½Π° Π²Π΅Π»ΠΈΡΠΈΠ½Ρ ΠΏΠΎΡΠ²Π΅Π½Π½ΠΎΠΉ ΡΠΌΠΈΡΡΠΈΠΈ. ΠΠΎΡΠ΅Π½ΡΠΈΠ°Π»ΡΠ½ΠΎΠ΅ ΡΠ²Π΅Π»ΠΈΡΠ΅Π½ΠΈΠ΅ ΠΏΠΎΡΠΎΠΊΠ° CO2 ΠΈΠ· ΠΏΠΎΡΠ²Ρ, Π²ΡΠ·Π²Π°Π½Π½ΠΎΠ΅ Π±ΡΠ΄ΡΡΠΈΠΌ ΡΠΎΡΡΠΎΠΌ ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΡ, ΠΌΠΎΠΆΠ΅Ρ Π²ΡΠ·Π²Π°ΡΡ ΡΡΡΠ΅ΠΊΡ ΠΏΠΎΠ»ΠΎΠΆΠΈΡΠ΅Π»ΡΠ½ΠΎΠΉ ΠΎΠ±ΡΠ°ΡΠ½ΠΎΠΉ ΡΠ²ΡΠ·ΠΈ Ρ ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΠ΅ΠΉ Π°ΡΠΌΠΎΡΡΠ΅ΡΠ½ΠΎΠ³ΠΎ CO2 ΠΈ Π³Π»ΠΎΠ±Π°Π»ΡΠ½ΡΠΌΠΈ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡΠΌΠΈ. ΠΠ»Ρ ΠΎΡΠ΅Π½ΠΊΠΈ Π±ΡΠ΄ΠΆΠ΅ΡΠΎΠ² C Π² Π·Π°Π΄Π°Π½Π½ΡΡ
ΡΠΊΠΎΡΠΈΡΡΠ΅ΠΌΠ°Ρ
ΠΌΡ Π΄ΠΎΠ»ΠΆΠ½Ρ ΡΠΌΠ΅ΡΡ ΠΎΠ±ΡΡΡΠ½ΠΈΡΡ ΠΌΠ΅Π»ΠΊΠΎΠΌΠ°ΡΡΡΠ°Π±Π½ΠΎΠ΅ ΠΏΡΠΎΡΡΡΠ°Π½ΡΡΠ²Π΅Π½Π½ΠΎΠ΅ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠ΅ ΠΏΠΎΡΠ²Π΅Π½Π½ΠΎΠ³ΠΎ Π΄ΡΡ
Π°Π½ΠΈΡ. ΠΠΎΠ΄Π΅Π»ΠΈ ΡΠ°ΡΡΠΈΡΠ΅Π»ΡΠ½ΠΎΡΡΠΈ ΡΡΠ΅Π±ΡΡΡ ΡΡΠ΅ΡΠ° ΠΊΠ°ΠΊ Π²ΡΠ΅ΠΌΠ΅Π½Π½ΠΎΠ³ΠΎ, ΡΠ°ΠΊ ΠΈ ΠΏΡΠΎΡΡΡΠ°Π½ΡΡΠ²Π΅Π½Π½ΠΎΠ³ΠΎ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡ Π΄ΡΡ
Π°Π½ΠΈΡ ΠΏΠΎΡΠ²Ρ ΠΈ ΠΌΠ°ΡΡΡΠ°Π±ΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΊΠ°ΠΌΠ΅ΡΠ½ΡΡ
ΠΈΠ·ΠΌΠ΅ΡΠ΅Π½ΠΈΠΉ Π΄ΡΡ
Π°Π½ΠΈΡ ΠΏΠΎΡΠ²Ρ Π΄ΠΎ ΡΡΠΎΠ²Π½Ρ ΡΠΊΠΎΡΠΈΡΡΠ΅ΠΌΡ. Π ΡΡΠΎΠΌ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΈ Π±ΡΠ»ΠΈ ΡΠΎΠΏΠΎΡΡΠ°Π²Π»Π΅Π½Ρ ΡΠ°Π·Π»ΠΈΡΠ½ΡΠ΅ ΠΏΠΎΠ΄ΡΡΠΈΠ»Π°ΡΡΠΈΠ΅ ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠΈ ΠΏΠΎ ΡΠΊΠΎΡΠΎΡΡΠΈ ΠΏΠΎΡΠ²Π΅Π½Π½ΠΎΠΉ ΡΠΌΠΈΡΡΠΈΠΈ ΠΈ ΠΎΠΏΡΠ΅Π΄Π΅Π»Π΅Π½Ρ ΠΎΡΠ½ΠΎΠ²Π½ΡΠ΅ ΡΠ°ΠΊΡΠΎΡΡ, Π² Π±ΠΎΠ»ΡΡΠ΅ ΡΡΠ΅ΠΏΠ΅Π½ΠΈ, Π²Π»ΠΈΡΡΡΠΈΠ΅ Π½Π° ΠΏΠΎΡΠΎΠΊΠΈ CO2 ΠΈΠ· ΠΏΠΎΡΠ²Ρ. ΠΡΠ»Π° ΡΠΎΠ·Π΄Π°Π½Π° ΠΌΠΎΠ΄Π΅Π»Ρ, ΠΊΠΎΡΠΎΡΠ°Ρ ΡΠΎΡΠ΅ΡΠ°Π΅Ρ Π² ΡΠ΅Π±Π΅ ΠΌΠ΅ΡΠ΅ΠΎΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΏΠ°ΡΠ°ΠΌΠ΅ΡΡΡ ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΈ ΠΈ ΠΌΠ΅ΡΡΠ½ΡΠ΅ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠΈ ΠΊΠ°ΠΆΠ΄ΠΎΠΉ ΡΠΊΠΎΡΠΈΡΡΠ΅ΠΌΡ
A Modified Algorithm for Estimating the Radial Cell Size in the Vaganov-Shashkin Simulation Model
ΠΠΎΠ½ΠΈΠΌΠ°Π½ΠΈΠ΅ ΠΌΠ΅Ρ
Π°Π½ΠΈΠ·ΠΌΠ° ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΈ ΡΠΎΡΡΠ° Π³ΠΎΠ΄ΠΈΡΠ½ΡΡ
ΠΊΠΎΠ»Π΅Ρ Π΄ΡΠ΅Π²Π΅ΡΠ½ΡΡ
ΡΠ°ΡΡΠ΅Π½ΠΈΠΉ ΠΏΠΎΠ΄
Π²Π»ΠΈΡΠ½ΠΈΠ΅ΠΌ Π²Π΅Π΄ΡΡΠΈΡ
ΡΠ°ΠΊΡΠΎΡΠΎΠ² Π²Π½Π΅ΡΠ½Π΅ΠΉ ΡΡΠ΅Π΄Ρ ΡΠ²Π»ΡΠ΅ΡΡΡ ΠΎΠ΄Π½ΠΎΠΉ ΠΈΠ· ΡΠ°ΠΌΡΡ
Π°ΠΊΡΡΠ°Π»ΡΠ½ΡΡ
ΠΏΡΠΎΠ±Π»Π΅ΠΌ
ΡΠΎΠ²ΡΠ΅ΠΌΠ΅Π½Π½ΠΎΠΉ Π΄Π΅Π½Π΄ΡΠΎΡΠΊΠΎΠ»ΠΎΠ³ΠΈΠΈ. Π£ΡΠΊΠΎΡΠ΅Π½ΠΈΠ΅ ΠΈΠ»ΠΈ Π·Π°ΠΌΠ΅Π΄Π»Π΅Π½ΠΈΠ΅ ΡΠΊΠΎΡΠΎΡΡΠΈ ΡΠΎΡΡΠ° Π΄Π΅ΡΠ΅Π²Π° Π² ΠΎΡΠ΄Π΅Π»ΡΠ½ΡΠ΅
ΠΈΠ½ΡΠ΅ΡΠ²Π°Π»Ρ ΡΠ΅Π·ΠΎΠ½Π° ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΠ΅ΡΡΡ ΡΠΎΠ²ΠΌΠ΅ΡΡΠ½ΡΠΌ Π²Π»ΠΈΡΠ½ΠΈΠ΅ΠΌ ΡΠ°ΠΊΠΈΡ
ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΠ°ΠΊΡΠΎΡΠΎΠ²,
ΠΊΠ°ΠΊ ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΠ° ΠΈ Π²Π»Π°ΠΆΠ½ΠΎΡΡΡ ΠΏΠΎΡΠ²Ρ. Π‘ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ΠΌ ΠΌΠΎΠ΄ΠΈΡΠΈΡΠΈΡΠΎΠ²Π°Π½Π½ΠΎΠ³ΠΎ Π°Π»Π³ΠΎΡΠΈΡΠΌΠ°
ΠΈΠΌΠΈΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠΉ ΠΌΠΎΠ΄Π΅Π»ΠΈ ΡΠΎΡΡΠ° Π΄ΡΠ΅Π²Π΅ΡΠ½ΡΡ
ΡΠ°ΡΡΠ΅Π½ΠΈΠΉ ΠΠ°Π³Π°Π½ΠΎΠ²Π°-Π¨Π°ΡΠΊΠΈΠ½Π° β VS-ΠΎΡΡΠΈΠ»Π»ΠΎΠ³ΡΠ°ΡΠ° β
Π² ΡΠ°Π±ΠΎΡΠ΅ ΠΌΠΎΠ΄Π΅Π»ΠΈΡΡΠ΅ΡΡΡ ΡΠ΅Π·ΠΎΠ½Π½ΡΠΉ ΡΠΎΡΡ ΠΊΠ»Π΅ΡΠΎΠΊ Π² Π³ΠΎΠ΄ΠΈΡΠ½ΠΎΠΌ ΠΊΠΎΠ»ΡΡΠ΅. ΠΡΠ΅Π΄Π»ΠΎΠΆΠ΅Π½ Π½ΠΎΠ²ΡΠΉ
ΠΌΠ°ΡΠ΅ΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΠΉ ΠΏΠΎΠ΄Ρ
ΠΎΠ΄ ΠΊ ΠΎΡΠ΅Π½ΠΊΠ΅ ΠΊΠ°ΠΌΠ±ΠΈΠ°Π»ΡΠ½ΠΎΠΉ Π°ΠΊΡΠΈΠ²Π½ΠΎΡΡΠΈ Ρ
Π²ΠΎΠΉΠ½ΡΡ
ΠΈ ΡΠ΅Π·ΠΎΠ½Π½ΠΎΠΉ ΠΊΠ»Π΅ΡΠΎΡΠ½ΠΎΠΉ
ΠΏΡΠΎΠ΄ΡΠΊΡΠΈΠΈ, ΠΊΠΎΡΠΎΡΡΠΉ Π±ΡΠ» ΠΏΡΠΎΡΠ΅ΡΡΠΈΡΠΎΠ²Π°Π½ Π½Π° ΠΎΠ±ΡΠ°Π·ΡΠ΅ ΡΠΎΡΠ½Ρ ΠΎΠ±ΡΠΊΠ½ΠΎΠ²Π΅Π½Π½ΠΎΠΉ (Pinus sylvestris L.),
ΠΎΡΠΎΠ±ΡΠ°Π½Π½ΠΎΠΌ Π² Π₯Π°ΠΊΠ°ΡΠΈΠΈ, Π·Π° ΠΏΠ΅ΡΠΈΠΎΠ΄ Ρ 1969 ΠΏΠΎ 2008 Π³Π³. ΠΠ»Π°Π³ΠΎΠ΄Π°ΡΡ Π΄Π°Π½Π½ΠΎΠΌΡ ΠΏΠΎΠ΄Ρ
ΠΎΠ΄Ρ ΡΠ΄Π°Π»ΠΎΡΡ
ΡΠ°Π·Π΄Π΅Π»ΠΈΡΡ Π²Π»ΠΈΡΠ½ΠΈΠ΅ ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈ Π½Π΅ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
Π²Π½Π΅ΡΠ½ΠΈΡ
ΡΠ°ΠΊΡΠΎΡΠΎΠ² Π½Π° ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅
ΠΊΠ»Π΅ΡΠΎΠΊ Π² Π³ΠΎΠ΄ΠΈΡΠ½ΠΎΠΌ ΠΊΠΎΠ»ΡΡΠ΅ Π΄ΡΠ΅Π²Π΅ΡΠ½ΡΡ
ΡΠ°ΡΡΠ΅Π½ΠΈΠΉTo describe the mechanism of tree-ring formation in woody plants influencing by the leading
environmental factors is one of the most urgent problems of modern dendroecology. Changing of
the tree-ring growth rate at selected intervals in the growing season is determined by the complex
influence of climatic factors (e.g. temperature and soil moisture). Using the modified algorithm of the
simulation model of growth Vaganov-Shashkin β VS-oscilloscope seasonal growth of cells in tree ring
is simulated in the work. New mathematical approach is developed to estimate a cambial activity
and seasonal cell production of conifer species. The approach is tested on tree-ring sample of Pinus
sylvestris for Khakassian region over 1969-2008. The obtained approach allows to separate a treering
growth signal on two components caused by climatic and non-climatic factor
Response of Four Tree Species to Changing Climate in a Moisture-Limited Area of South Siberia
Forward Modeling Reveals Multidecadal Trends in Cambial Kinetics and Phenology at Treeline
Significant alterations of cambial activity might be expected due to climate warming, leading to growing season extension and higher growth rates especially in cold-limited forests. However, assessment of climate-change-driven trends in intra-annual wood formation suffers from the lack of direct observations with a timespan exceeding a few years. We used the Vaganov-Shashkin process-based model to: (i) simulate daily resolved numbers of cambial and differentiating cells; and (ii) develop chronologies of the onset and termination of specific phases of cambial phenology during 1961β2017. We also determined the dominant climatic factor limiting cambial activity for each day. To asses intra-annual model validity, we used 8 years of direct xylogenesis monitoring from the treeline region of the KrkonoΕ‘e Mts. (Czechia). The model exhibits high validity in case of spring phenological phases and a seasonal dynamics of tracheid production, but its precision declines for estimates of autumn phenological phases and growing season duration. The simulations reveal an increasing trend in the number of tracheids produced by cambium each year by 0.42 cells/year. Spring phenological phases (onset of cambial cell growth and tracheid enlargement) show significant shifts toward earlier occurrence in the year (for 0.28β0.34 days/year). In addition, there is a significant increase in simulated growth rates during entire growing season associated with the intra-annual redistribution of the dominant climatic controls over cambial activity. Results suggest that higher growth rates at treeline are driven by (i) temperature-stimulated intensification of spring cambial kinetics, and (ii) decoupling of summer growth rates from the limiting effect of low summer temperature due to higher frequency of climatically optimal days. Our results highlight that the cambial kinetics stimulation by increasing spring and summer temperatures and shifting spring phenology determine the recent growth trends of treeline ecosystems. Redistribution of individual climatic factors controlling cambial activity during the growing season questions the temporal stability of climatic signal of cold forest chronologies under ongoing climate change
Response of four tree species to changing climate in 2 a moisture-limited area of South Siberia
The response of vegetation to climate change is of special interest in regions where rapid warming is coupled with moisture deficit. This raises the question of the limits in plants' acclimation ability and the consequent shifts of the vegetation cover. Radial growth dynamics and climatic response were studied in Scots pine (Pinus sylvestris L.), Siberian larch (Larix sibirica Ledeb.), and silver birch (Betula pendula Roth.) in the forest-steppe, and for Siberian elm (Ulmus pumila L.) in the steppe of South Siberia, as indicators of vegetation state and dynamics. Climate-growth relationships were analyzed by the following two approaches: (1) correlations between tree-ring width chronologies and short-term moving climatic series, and (2) optimization of the parameters of the Vaganov-Shashkin tree growth simulation model to assess the ecophysiological characteristics of species. Regional warming was accompanied by a slower increase of the average moisture deficit, but not in the severity of droughts. In the forest-steppe, the trees demonstrated stable growth and responded to the May-July climate. In the steppe, elm was limited by moisture deficit in May-beginning of June, during the peak water deficit. The forest-steppe stands were apparently acclimated successfully to the current climatic trends. It seems that elm was able to counter the water deficit, likely through its capacity to regulate transpiration by the stomatal morphology and xylem structure, using most of the stem as a water reservoir; earlier onset; and high growth rate, and these physiological traits may provide advantages to this species, leading to its expansion in steppes
Visual Parameterization of Vaganov-Shashkin Simulation Model and its Application in Dendroecological Research
Π Π΄Π΅Π½Π΄ΡΠΎΡ
ΡΠΎΠ½ΠΎΠ»ΠΎΠ³ΠΈΠΈ ΠΈΡΠΏΠΎΠ»ΡΠ·ΡΠ΅ΡΡΡ Π±ΠΎΠ»ΡΡΠΎΠ΅ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²ΠΎ ΡΠ°Π·Π»ΠΈΡΠ½ΡΡ
Π°Π½Π°Π»ΠΈΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΏΠΎΠ΄Ρ
ΠΎΠ΄ΠΎΠ²
Π΄Π»Ρ Π°Π½Π°Π»ΠΈΠ·Π° Π΄Π°Π½Π½ΡΡ
, ΠΎΠ΄Π½ΠΈΠΌ ΠΈΠ· ΠΊΠΎΡΠΎΡΡΡ
ΡΠ²Π»ΡΠ΅ΡΡΡ ΠΌΠΎΠ΄Π΅Π»ΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅. ΠΡΠΈ ΡΠΎΠ·Π΄Π°Π½ΠΈΠΈ Π»ΡΠ±ΠΎΠΉ ΠΌΠΎΠ΄Π΅Π»ΠΈ
ΠΎΠ΄Π½ΠΈΠΌ ΠΈΠ· Π³Π»Π°Π²Π½ΡΡ
Π²ΠΎΠΏΡΠΎΡΠΎΠ² Π²ΡΡΡΡΠΏΠ°Π΅Ρ Π²ΡΠ±ΠΎΡ Π³Π»Π°Π²Π½ΡΡ
ΡΠ°ΠΊΡΠΎΡΠΎΠ². Π‘Π°ΠΌΡΠ΅ ΡΠ°ΡΠΏΡΠΎΡΡΡΠ°Π½Π΅Π½Π½ΡΠ΅ ΠΈ
Π΄ΠΎΡΡΡΠΏΠ½ΡΠ΅ ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ Π΄Π°Π½Π½ΡΠ΅ β ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΠ° ΠΈ ΠΎΡΠ°Π΄ΠΊΠΈ.
ΠΠ° ΠΎΡΠ½ΠΎΠ²Π°Π½ΠΈΠΈ ΠΈΠΌΠΈΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠΉ ΠΌΠΎΠ΄Π΅Π»ΠΈ ΠΠ°Π³Π°Π½ΠΎΠ²Π°-Π¨Π°ΡΠΊΠΈΠ½Π° ΠΏΡΠ΅Π΄Π»ΠΎΠΆΠ΅Π½ Π½ΠΎΠ²ΡΠΉ Π°Π»Π³ΠΎΡΠΈΡΠΌ
Π²ΠΈΠ·ΡΠ°Π»ΡΠ½ΠΎΠΉ ΠΏΠ°ΡΠ°ΠΌΠ΅ΡΡΠΈΠ·Π°ΡΠΈΠΈ ΡΠΎΡΡΠ° Π³ΠΎΠ΄ΠΈΡΠ½ΡΡ
ΠΊΠΎΠ»Π΅Ρ Ρ
Π²ΠΎΠΉΠ½ΡΡ
Π΄Π΅ΡΠ΅Π²ΡΠ΅Π², Π½Π°Π·Π²Π°Π½Π½ΡΠΉ Β«VS-
ΠΎΡΡΠΈΠ»Π»ΠΎΠ³ΡΠ°ΡΒ», ΠΈ ΠΎΠΏΠΈΡΠ°Π½Π° Π΅Π³ΠΎ ΠΏΡΠΎΠ³ΡΠ°ΠΌΠΌΠ½Π°Ρ ΡΠ΅Π°Π»ΠΈΠ·Π°ΡΠΈΡ. ΠΠΎΠ»ΡΡΠ΅Π½Π½ΡΠΉ Π°Π»Π³ΠΎΡΠΈΡΠΌ Π±ΡΠ»
Π°ΠΏΡΠΎΠ±ΠΈΡΠΎΠ²Π°Π½ Π½Π° Π΄Π²ΡΡ
ΠΏΠΎΡΠΎΠ΄Π°Ρ
Π΄ΡΠ΅Π²Π΅ΡΠ½ΡΡ
ΡΠ°ΡΡΠ΅Π½ΠΈΠΉ β Larix gmelini ΠΈ Picea obovata. ΠΠΎΠ²ΡΠΉ ΡΠΏΠΎΡΠΎΠ±
ΠΏΠ°ΡΠ°ΠΌΠ΅ΡΡΠΈΠ·Π°ΡΠΈΠΈ ΠΈ Π°Π½Π°Π»ΠΈΠ· ΠΌΠΎΠ΄Π΅Π»ΠΈΡΡΠ΅ΠΌΡΡ
ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΠΎΠ² ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡΡ ΠΎΡΠ΅Π½ΠΈΡΡ Π»ΠΎΠΊΠ°Π»ΡΠ½ΡΠ΅ ΡΡΠ»ΠΎΠ²ΠΈΡ
ΠΏΡΠΎΠΈΠ·ΡΠ°ΡΡΠ°Π½ΠΈΡ Π΄ΡΠ΅Π²Π΅ΡΠ½ΡΡ
ΡΠ°ΡΡΠ΅Π½ΠΈΠΉ Π½Π° ΠΎΡΠ½ΠΎΠ²Π΅ Π΄ΠΈΠ½Π°ΠΌΠΈΠΊΠΈ Π΄Π²ΡΡ
ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΏΠ΅ΡΠ΅ΠΌΠ΅Π½Π½ΡΡ
:
ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΡ ΠΈ ΠΎΡΠ°Π΄ΠΊΠΎΠ², Π±Π΅Π· ΠΏΡΠΈΠ²Π»Π΅ΡΠ΅Π½ΠΈΡ Π΄ΠΎΠΏΠΎΠ»Π½ΠΈΡΠ΅Π»ΡΠ½ΠΎΠΉ ΠΈΠ½ΡΠΎΡΠΌΠ°ΡΠΈΠΈ ΠΎ ΠΌΠ΅ΡΡΠΎΠΎΠ±ΠΈΡΠ°Π½ΠΈΠΈThere are many different methods and tools for data analysis in dendrochronology. Modeling is one of
them. One of the main issues in modeling is a choice of the main factors. Π‘limatic data (temperature
and precipitation) are the most common and affordable of them. Based on Vaganov β Shaskin model
the new algorithm of visual parameterization of three-ring growth β VS-oscilloscope was developed.
Algorithm was tested on different species of woody plants β Larix gmelini and Picea obovata. A new
parameterization and analysis of modeling results help to evaluate conditions of area of growth of
woody plants, based on dynamic of two climate variables: temperature and precipitation, without
adding information about area of growt