RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 17, ES4002, doi:10.2205/2017ES000605, 2017


Table 1. Meteorological measurements on Djankuat glacier in 2007–2016 and their accuracy
Data sourceMeasured value and its accuracy (modulus) Period of
measurements (with
number of days
in brackets)
Sampling
interval
Air
temperature
$T$, ° C
Relative
humidity
$F$, %
Wind
speed $V$,
m/s
Components of
radiation balance
$B$, W/m$^2$
Distance
"sensor-
surface" $H$, m
15.06.07–30.09.07 (107)
17.06.08–30.09.08 (105)
01.07.09–30.09.09 (91)
09.07.10–29.09.10 (82)
AWS 0.25 0.5–215 0.04–0.06 10.07.12–05.08.12 (26) 15 min
CAMPBELL 07.07.13–09.09.13 (64)
19.06.14–30.09.14 (103)
07.07.15–04.09.15 (59)
20.06.16–05.09.16 (77)
Gradient mast 0.4 100.5–2 05.07.15–15.08.15 (41) 15 min
DAVIS
12.07.13–03.08.13
Sonic 09.08.13–16.08.13
anemometer 0.05–0.1 0.01–0.0526.08.13–06.09.13 (42) 0.1 s
GILL 30.06.14–30.07.14 (30)
17.06.16–01.08.16 (45)

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Citation: Toropov P. A., A. A. Shestakova, A. M. Smirnov (2017), Methodological aspects of heat balance components estimation on mountain glaciers, Russ. J. Earth Sci., 17, ES4002, doi:10.2205/2017ES000605.


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