Zobrazeno 1 - 8
of 8
pro vyhledávání: '"I. L. Kalyuzhnyi"'
Autor:
I. L. Kalyuzhnyi
Publikováno v:
Russian Meteorology and Hydrology. 47:668-676
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d682dc5e831a5cecd47b9cf76104e0a1
https://doi.org/10.3103/s1068373922090047
https://doi.org/10.3103/s1068373922090047
Autor:
S. A. Lavrov, I. L. Kalyuzhnyi
Publikováno v:
Water Resources. 44:604-613
The depth of soil freezing in river watersheds is a factor governing winter runoff formation. The freezing depth regulates the redistribution of stored soil moisture between thawed and frozen soil layers. The moisture stored in the thawed soil layer
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::815fe397b42adbe7f133da056b05ee52
https://doi.org/10.1134/s0097807817040078
https://doi.org/10.1134/s0097807817040078
Autor:
I. L. Kalyuzhnyi, S. A. Lavrov
Publikováno v:
Russian Meteorology and Hydrology. 41:487-496
The results of the analysis of spatiotemporal variability of frost depth in the Volga River basin are presented. It is demonstrated that in the geographic zones of the basin the mean frost depth decreased in wide limits: from 10-20 to 90-100 cm and m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7d869f5d38b594bcf7e4dbe54d7090f7
https://doi.org/10.3103/s1068373916070062
https://doi.org/10.3103/s1068373916070062
Autor:
I. L. Kalyuzhnyi, S. A. Lavrov
Publikováno v:
Russian Meteorology and Hydrology. 37:47-56
A mechanism of climate change influence on the Medvenka River runoff in the winter- and springtime is revealed based on the generalized long-term observations carried out at the Podmoskovnaya water-balance station. It is demonstrated that average inc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::16883a83318e6ef426b516df319e107e
https://doi.org/10.3103/s1068373912010074
https://doi.org/10.3103/s1068373912010074
Publikováno v:
Water Resources. 39:44-55
The mechanism and factors of the impact of climate changes on the level regime of bog water and the runoff from bogs has been established.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::721e4e142dc6530179a91c2bd5ca67cd
https://doi.org/10.1134/s0097807812010046
https://doi.org/10.1134/s0097807812010046
Autor:
K. D. Romanyuk, I. L. Kalyuzhnyi
Publikováno v:
Russian Meteorology and Hydrology. 35:490-499
A considerable variation of hydrological regime of oligotrophic bogs of northern and northwestern Russia takes place during all phases of hydrological year under influence of climatic changes of recent decades. The mechanism and factors of climate ch
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::604c28e258bd9ab7c2e1416a3c56d7da
https://doi.org/10.3103/s1068373910070095
https://doi.org/10.3103/s1068373910070095
Publikováno v:
Russian Meteorology and Hydrology. 34:35-45
Results of measuring methane emissions from the Lammin-Suo oligotrophic bog massif are considered. It is shown that emission intensity depends on the methane transport from the active layer of the peat bed. The highest emission intensity is observed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e2fe872ae8f94020a6d3758cbd1578f2
https://doi.org/10.3103/s1068373909010063
https://doi.org/10.3103/s1068373909010063
Autor:
K. K. Pavlova, I. L. Kalyuzhnyi
Publikováno v:
Hydrotechnical Construction. 14:375-379
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6e772832676912f2c5c3d7766e87ed12
https://doi.org/10.1007/bf02305281
https://doi.org/10.1007/bf02305281