ON THE NONSTATIONARITY OF DEEP BAIKAL WAT ER FLOWS AS DERIVED FROM NEUTRINO TELESCOPE DATA

Authors
BELOLAPTIKOV IA BEZRUKOV LB BORISOVETS BA BUDNEV NM VIEBUSH K WISCHNEWSKI A GAPONENKO ON GARUS AA GRESS OA GRESS TI DANILCHENKO IA DZHILKIBAEV ZAM DOBRYNIN VI DOMOGATSKII GV DOROSHENKO AA IGNATEV SB KARLE A KLABUKOV AM KLIMOV AI KLIMUSHKIN SI KOSHECHKIN AP KULEPOV VF KUZMICHEV LA LOVTSOV SV LUBSANDORZHIEV BK MAKSIMOV VN MAKSIMOVA EA MILENIN MB MIKOLAJSKI T MIRGAZOV RR MOSEIKO NI MOROZ AV NIKIFOROV SA OSIPOVA EM PAVLOV AA PANFILOV AI PARFENOV YV PETUKHOV DP POKOLEV PA POCHEIKIN KA POKHIL PG ROZANOV MI PUBTSOV VY SINEGOVSKII SI SOKALSKII IA TARASHCHANSKII BA THON T FIALKOVSKII SV HEUKENKAMP H CHENSKII AG SPIERING C STREYCHER O
Citation
Ia. Belolaptikov et al., ON THE NONSTATIONARITY OF DEEP BAIKAL WAT ER FLOWS AS DERIVED FROM NEUTRINO TELESCOPE DATA, Izvestia Akademii nauk. Rossijskaa akademia nauk. Fizika atmosfery iokeana, 34(1), 1998, pp. 90-96
Citations number
12
Categorie Soggetti
Metereology & Atmospheric Sciences",Oceanografhy
Journal title
Izvestia Akademii nauk. Rossijskaa akademia nauk. Fizika atmosfery iokeana → ACNP
ISSN journal
10236317
Volume
34
Issue
1
Year of publication
1998
Pages
90 - 96
Database
ISI
SICI code
1023-6317(1998)34:1<90:OTNODB>2.0.ZU;2-3
Abstract
Data on the luminescence of the Baikal water medium that have been obt ained with the neutrino telescope NT-36 are presented. The maximum lev el of luminescence and its high spatial and temporal inhomogeneity are observed annually from August to October. This is explained by the no nstationary processes of water inflow from shallow depths with high ve rtical velocities. A case when the velocity of vertical water motion w as equal to 2.3 cm s(-1) is described. The important role of dynamic f actors in initializing the vertical water exchange is underlined.