360
Land-Ocean SYstems in the Siberian Arctic: Dynamics and History
Q[mJ .. n
10 22. 24 16 18 '0 OL 04 06 08 10 " Il IS 17 19 21 . lJ 1S 17 29 II 02 ()4 06 ot 09 " I) IS
~~~~~~~wwwww~ww~wwwwww
_______ _
o
100
1-«)
10
120
100
30
60
.0
40
20
Figure 6: Krasnaya Hydrograph 1995 and precipitation.
They accumulate in several river deltas and in the lake's deep-water zones, and are not
exported outside. The lake's sediment output in the summertime has no significant variations
and the variability over several years is very small.
S The thermal regime of the lake's tributaries and the outflow river differs significantly. The
water temperature of the lake's tributaries is closely connected to the air temperature
variations, both within a day and over the entire season. The water temperature of the
Protochny is governed by the thermal regime of the lake, and does not depend on the daily
air temperature variations.
6 The complete water exchange of the Levinson-Lessing-Lake occurs within 9 to 10 years.
References
B1ey, D. and K.-H. Schmidt (1994) Schwebstofferfassung tiber die Trtibungsmessung in einem Wildbach
(Lainbach, Oberbayern). In: Messungen in fluvialen Systemen. Feld- und Labormethoden zur Erfassung des
Wasser- und Stoffhaushaltes, Barsch, D., R. Mausbacher, K.-H. Piirtge and K.-H. Schmidt (Hrsg).
Siegert, C. and D. Bolshiyanov (1995) Russian-German Cooperation: The Expedition TAYMYR 1994. Berichte
zur Polarforschung 175.
Schmidt, K.-H., D. Bley, R. Busskamp and D. Gintz (1992) Feststofftransport und FluBbettdynamik in
Wildbachsystemen. Das Beispiel des Lainbachs in Oberbayern. Die Erde, 123.
Land-Ocean SYstems in the Siberian Arctic: Dynamics and History
Q[mJ .. n
10 22. 24 16 18 '0 OL 04 06 08 10 " Il IS 17 19 21 . lJ 1S 17 29 II 02 ()4 06 ot 09 " I) IS
~~~~~~~wwwww~ww~wwwwww
_______ _
o
100
1-«)
10
120
100
30
60
.0
40
20
Figure 6: Krasnaya Hydrograph 1995 and precipitation.
They accumulate in several river deltas and in the lake's deep-water zones, and are not
exported outside. The lake's sediment output in the summertime has no significant variations
and the variability over several years is very small.
S The thermal regime of the lake's tributaries and the outflow river differs significantly. The
water temperature of the lake's tributaries is closely connected to the air temperature
variations, both within a day and over the entire season. The water temperature of the
Protochny is governed by the thermal regime of the lake, and does not depend on the daily
air temperature variations.
6 The complete water exchange of the Levinson-Lessing-Lake occurs within 9 to 10 years.
References
B1ey, D. and K.-H. Schmidt (1994) Schwebstofferfassung tiber die Trtibungsmessung in einem Wildbach
(Lainbach, Oberbayern). In: Messungen in fluvialen Systemen. Feld- und Labormethoden zur Erfassung des
Wasser- und Stoffhaushaltes, Barsch, D., R. Mausbacher, K.-H. Piirtge and K.-H. Schmidt (Hrsg).
Siegert, C. and D. Bolshiyanov (1995) Russian-German Cooperation: The Expedition TAYMYR 1994. Berichte
zur Polarforschung 175.
Schmidt, K.-H., D. Bley, R. Busskamp and D. Gintz (1992) Feststofftransport und FluBbettdynamik in
Wildbachsystemen. Das Beispiel des Lainbachs in Oberbayern. Die Erde, 123.