8 research outputs found
Dynamic-stochastic modeling of snow cover formation on the European territory of Russia
A dynamic-stochastic model, which combines a deterministic model of snow cover formation with a stochastic weather generator, has been developed. The deterministic snow model describes temporal change of the snow depth, content of ice and liquid water, snow density, snowmelt, sublimation, re-freezing of melt water, and snow metamorphism. The model has been calibrated and validated against the long-term data of snow measurements over the territory of the European Russia. The model showed good performance in simulating time series of the snow water equivalent and snow depth. The developed weather generator (NEsted Weather Generator, NewGen) includes nested generators of annual, monthly and daily time series of weather variables (namely, precipitation, air temperature, and air humidity). The parameters of the NewGen have been adjusted through calibration against the long-term meteorological data in the European Russia. A disaggregation procedure has been proposed for transforming parameters of the annual weather generator into the parameters of the monthly one and, subsequently, into the parameters of the daily generator. Multi-year time series of the simulated daily weather variables have been used as an input to the snow model. Probability properties of the snow cover, such as snow water equivalent and snow depth for return periods of 25 and 100 years, have been estimated against the observed data, showing good correlation coefficients. The described model has been applied to different landscapes of European Russia, from steppe to taiga regions, to show the robustness of the proposed technique
ΠΠΈΠ½Π°ΠΌΠΈΠΊΠΎ-ΡΡΠΎΡ Π°ΡΡΠΈΡΠ΅ΡΠΊΠΎΠ΅ ΠΌΠΎΠ΄Π΅Π»ΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΡΠ½Π΅ΠΆΠ½ΠΎΠ³ΠΎ ΠΏΠΎΠΊΡΠΎΠ²Π° Π½Π° ΠΠ²ΡΠΎΠΏΠ΅ΠΉΡΠΊΠΎΠΉ ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΈ Π ΠΎΡΡΠΈΠΈ
A dynamic-stochastic model, which combines a deterministic model of snow cover formation with a stochastic weather generator, has been developed. The deterministic snow model describes temporal change of the snow depth, content of ice and liquid water, snow density, snowmelt, sublimation, re-freezing of melt water, and snow metamorphism. The model has been calibrated and validated against the long-term data of snow measurements over the territory of the European Russia. The model showed good performance in simulating time series of the snow water equivalent and snow depth. The developed weather generator (NEsted Weather Generator, NewGen) includes nested generators of annual, monthly and daily time series of weather variables (namely, precipitation, air temperature, and air humidity). The parameters of the NewGen have been adjusted through calibration against the long-term meteorological data in the European Russia. A disaggregation procedure has been proposed for transforming parameters of the annual weather generator into the parameters of the monthly one and, subsequently, into the parameters of the daily generator. Multi-year time series of the simulated daily weather variables have been used as an input to the snow model. Probability properties of the snow cover, such as snow water equivalent and snow depth for return periods of 25 and 100 years, have been estimated against the observed data, showing good correlation coefficients. The described model has been applied to different landscapes of European Russia, from steppe to taiga regions, to show the robustness of the proposed technique.Β Π Π°Π·ΡΠ°Π±ΠΎΡΠ°Π½Π° Π΄ΠΈΠ½Π°ΠΌΠΈΠΊΠΎ-ΡΡΠΎΡ
Π°ΡΡΠΈΡΠ΅ΡΠΊΠ°Ρ ΠΌΠΎΠ΄Π΅Π»Ρ, ΠΊΠΎΠΌΠΏΠΎΠ½Π΅Π½ΡΡ ΠΊΠΎΡΠΎΡΠΎΠΉ β Π΄Π΅ΡΠ΅ΡΠΌΠΈΠ½ΠΈΡΡΠΈΡΠ΅ΡΠΊΠ°Ρ ΠΌΠΎΠ΄Π΅Π»Ρ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΡΠ½Π΅ΠΆΠ½ΠΎΠ³ΠΎ ΠΏΠΎΠΊΡΠΎΠ²Π° ΠΈ ΡΡΠΎΡ
Π°ΡΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΌΠΎΠ΄Π΅Π»ΠΈ Π²ΡΠ΅ΠΌΠ΅Π½Π½ΡΜΡ
ΡΡΠ΄ΠΎΠ² Π²Ρ
ΠΎΠ΄Π½ΡΡ
ΠΌΠ΅ΡΠ΅ΠΎΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
Π²Π΅Π»ΠΈΡΠΈΠ½ (ΡΡΠΎΡ
Π°ΡΡΠΈΡΠ΅ΡΠΊΠΈΠΉ Π³Π΅Π½Π΅ΡΠ°ΡΠΎΡ ΠΏΠΎΠ³ΠΎΠ΄Ρ). ΠΠ΅ΡΠ΅ΡΠΌΠΈΠ½ΠΈΡΡΠΈΡΠ΅ΡΠΊΠ°Ρ ΠΌΠΎΠ΄Π΅Π»Ρ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΡΠ½Π΅ΠΆΠ½ΠΎΠ³ΠΎ ΠΏΠΎΠΊΡΠΎΠ²Π° ΠΎΠΏΠΈΡΡΠ²Π°Π΅Ρ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡ Π²ΠΎ Π²ΡΠ΅ΠΌΠ΅Π½ΠΈ ΡΠΎΠ»ΡΠΈΠ½Ρ ΡΠ½Π΅Π³Π°, ΡΠΎΠ΄Π΅ΡΠΆΠ°Π½ΠΈΡ Π»ΡΠ΄Π° ΠΈ ΡΠ°Π»ΠΎΠΉ Π²ΠΎΠ΄Ρ Π² Π½ΡΠΌ, ΠΏΡΠΎΡΠ΅ΡΡΡ ΡΠ½Π΅Π³ΠΎΡΠ°ΡΠ½ΠΈΡ, ΡΡΠ±Π»ΠΈΠΌΠ°ΡΠΈΠΈ ΠΈ Π·Π°ΠΌΠ΅ΡΠ·Π°Π½ΠΈΡ ΡΠ°Π»ΠΎΠΉ Π²ΠΎΠ΄Ρ Π² ΡΠΎΠ»ΡΠ΅ ΡΠ½Π΅Π³Π°. ΠΠ°Π»ΠΈΠ±ΡΠΎΠ²ΠΊΠ° ΠΌΠΎΠ΄Π΅Π»ΠΈ ΠΏΠΎ Π΄Π°Π½Π½ΡΠΌ ΠΌΠ½ΠΎΠ³ΠΎΠ»Π΅ΡΠ½ΠΈΡ
Π½Π°Π±Π»ΡΠ΄Π΅Π½ΠΈΠΉ Π·Π° ΡΠ½Π΅ΠΆΠ½ΡΠΌ ΠΏΠΎΠΊΡΠΎΠ²ΠΎΠΌ Π½Π° 36 ΠΌΠ΅ΡΠ΅ΠΎΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΡΠ°Π½ΡΠΈΡΡ
Π½Π° ΠΠ²ΡΠΎΠΏΠ΅ΠΉΡΠΊΠΎΠΉ ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΈ Π ΠΎΡΡΠΈΠΈ ΠΏΠΎΠ·Π²ΠΎΠ»ΠΈΠ»Π° ΠΏΠΎΠ»ΡΡΠΈΡΡ Π°Π΄Π΅ΠΊΠ²Π°ΡΠ½ΡΠ΅ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΏΠΎ Π²ΠΎΡΠΏΡΠΎΠΈΠ·Π²Π΅Π΄Π΅Π½ΠΈΡ Π·Π°ΠΏΠ°ΡΠΎΠ² Π²ΠΎΠ΄Ρ Π² ΡΠ½Π΅ΠΆΠ½ΠΎΠΌ ΠΏΠΎΠΊΡΠΎΠ²Π΅ ΠΈ ΡΠΎΠ»ΡΠΈΠ½Ρ ΡΠ½Π΅Π³Π°. Π Π°Π·ΡΠ°Π±ΠΎΡΠ°Π½ ΡΡΠΎΡ
Π°ΡΡΠΈΡΠ΅ΡΠΊΠΈΠΉ Π³Π΅Π½Π΅ΡΠ°ΡΠΎΡ ΠΏΠΎΠ³ΠΎΠ΄Ρ (NEsted Weather Generator, NEWGen) Π΄Π»Ρ ΠΌΠΎΠ΄Π΅Π»ΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΌΠ΅ΡΠΎΠ΄ΠΎΠΌ ΠΠΎΠ½ΡΠ΅-ΠΠ°ΡΠ»ΠΎ ΠΌΠ½ΠΎΠ³ΠΎΠ»Π΅ΡΠ½ΠΈΡ
Π²ΡΠ΅ΠΌΠ΅Π½Π½ΡΜΡ
ΡΡΠ΄ΠΎΠ² ΡΡΠ΅Π΄Π½Π΅ΡΡΡΠΎΡΠ½ΡΡ
Π·Π½Π°ΡΠ΅Π½ΠΈΠΉ ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΡ Π²ΠΎΠ·Π΄ΡΡ
Π°, ΠΎΡΠ°Π΄ΠΊΠΎΠ² ΠΈ Π²Π»Π°ΠΆΠ½ΠΎΡΡΠΈ Π²ΠΎΠ·Π΄ΡΡ
Π°, ΠΊΠΎΡΠΎΡΡΠ΅ ΠΏΡΠ΅Π΄ΡΡΠ°Π²Π»ΡΡΡ ΡΠΎΠ±ΠΎΠΉ Π²Ρ
ΠΎΠ΄Π½ΡΠ΅ ΠΏΠ΅ΡΠ΅ΠΌΠ΅Π½Π½ΡΠ΅ Π΄Π΅ΡΠ΅ΡΠΌΠΈΠ½ΠΈΡΡΠΈΡΠ΅ΡΠΊΠΎΠΉ ΠΌΠΎΠ΄Π΅Π»ΠΈ. ΠΠ»Ρ ΠΎΡΠ΅Π½ΠΊΠΈ ΠΏΠ°ΡΠ°ΠΌΠ΅ΡΡΠΎΠ² ΠΈ ΠΏΡΠΎΠ²Π΅ΡΠΊΠΈ ΡΡΠΎΡ
Π°ΡΡΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ Π³Π΅Π½Π΅ΡΠ°ΡΠΎΡΠ° ΠΏΠΎΠ³ΠΎΠ΄Ρ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π»ΠΈ Π΄Π°Π½Π½ΡΠ΅ ΠΌΠ½ΠΎΠ³ΠΎΠ»Π΅ΡΠ½ΠΈΡ
Π½Π°Π±Π»ΡΠ΄Π΅Π½ΠΈΠΉ Π½Π° ΠΌΠ΅ΡΠ΅ΠΎΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΡΠ°Π½ΡΠΈΡΡ
ΠΠ²ΡΠΎΠΏΠ΅ΠΉΡΠΊΠΎΠΉ ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΈ Π ΠΎΡΡΠΈΠΈ. Π’ΡΡΡΡΠ΅Π»Π΅ΡΠ½ΠΈΠ΅ ΡΡΠ΄Ρ ΠΌΠ΅ΡΠ΅ΠΎΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
Π²Π΅Π»ΠΈΡΠΈΠ½, ΡΠ³Π΅Π½Π΅ΡΠΈΡΠΎΠ²Π°Π½Π½ΡΠ΅ ΠΌΠ΅ΡΠΎΠ΄ΠΎΠΌ ΠΠΎΠ½ΡΠ΅-ΠΠ°ΡΠ»ΠΎ, Π·Π°Π΄Π°Π²Π°Π»ΠΈΡΡ Π² ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅ Β«Π²Ρ
ΠΎΠ΄ΠΎΠ²Β» Π² ΠΌΠΎΠ΄Π΅Π»Ρ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΡΠ½Π΅ΠΆΠ½ΠΎΠ³ΠΎ ΠΏΠΎΠΊΡΠΎΠ²Π°, Ρ ΠΏΠΎΠΌΠΎΡΡΡ ΠΊΠΎΡΠΎΡΠΎΠΉ ΡΠ°ΡΡΡΠΈΡΡΠ²Π°Π»ΠΈΡΡ ΡΡΠ΄Ρ ΡΠΎΠ»ΡΠΈΠ½Ρ ΡΠ½Π΅Π³Π° ΠΈ ΡΠ½Π΅Π³ΠΎΠ·Π°ΠΏΠ°ΡΠΎΠ² ΠΈ ΠΎΡΠ΅Π½ΠΈΠ²Π°Π»ΠΈΡΡ ΠΈΡ
Π²Π΅ΡΠΎΡΡΠ½ΠΎΡΡΠ½ΡΠ΅ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠΈ. ΠΠΎΠ»ΡΡΠ΅Π½ΠΎ ΡΠ΄ΠΎΠ²Π»Π΅ΡΠ²ΠΎΡΠΈΡΠ΅Π»ΡΠ½ΠΎΠ΅ ΡΠΎΠΎΡΠ²Π΅ΡΡΡΠ²ΠΈΠ΅ ΡΡΠ°ΡΠΈΡΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΏΠ°ΡΠ°ΠΌΠ΅ΡΡΠΎΠ², ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΠ½Π½ΡΡ
ΠΏΠΎ ΡΠ°ΠΊΡΠΈΡΠ΅ΡΠΊΠΈΠΌ ΠΈ ΡΠ°ΡΡΡΠΈΡΠ°Π½Π½ΡΠΌ ΡΡΠ΄Π°ΠΌ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊ ΡΠ½Π΅ΠΆΠ½ΠΎΠ³ΠΎ ΠΏΠΎΠΊΡΠΎΠ²Π°
Ensemble seasonal forecast of extreme water inflow into a large reservoir
An approach to seasonal ensemble forecast of unregulated water inflow into a
large reservoir was developed. The approach is founded on a physically-based
semi-distributed hydrological model ECOMAG driven by Monte-Carlo generated
ensembles of weather scenarios for a specified lead-time of the forecast
(3 months ahead in this study). Case study was carried out for the Cheboksary
reservoir (catchment area is 374 000 km2) located on the middle Volga
River. Initial watershed conditions on the forecast date (1 March
for spring freshet and 1 June for summer low-water period) were
simulated by the hydrological model forced by daily meteorological
observations several months prior to the forecast date. A spatially
distributed stochastic weather generator was used to produce time-series of
daily weather scenarios for the forecast lead-time. Ensemble of daily water
inflow into the reservoir was obtained by driving the ECOMAG model with the
generated weather time-series. The proposed ensemble forecast technique was
verified on the basis of the hindcast simulations for 29 spring and summer
seasons beginning from 1982 (the year of the reservoir filling to capacity)
to 2010. The verification criteria were used in order to evaluate an ability
of the proposed technique to forecast freshet/low-water events of the
pre-assigned severity categories