|
CALM SITE R19 |
LAKE GLUKHOE |
|
Site code |
R19 |
|
Site name |
Lake
Glukhoe |
|
CAPS I Metadata form |
GGD362 |
|
CAPS II Metadata form |
GGD313_R19 |
|
Responsible for data submission |
David
Gilichinsky |
|
Email Address |
gilichin@online.stack.ru |
|
Institution/Organization |
Institute
of Physicochemical and Biological Problems in Soil Science Pushchino, Moscow
region |
|
Location description |
Lower Kolyma
River |
|
Location Lat. |
68 deg. 48
min. N |
|
Location Lon. |
160 deg. 57
min. E |
|
Elevation avg. (m) |
15 |
|
Methods Grid |
100 |
|
Methods Other |
|
|
Landscape Description |
Sandy plain
with lakes |
|
Vegetation /Classification |
Thin larch
forest |
|
Soils (or Material) |
Turbic
Cryosols (sandy) |
|
Thaw depth measurements (year started)
|
1996 |
|
Air temp. measurements (year started) |
|
|
Snow cover measurements (year started) |
|
|
soil temp. measurements (year started) |
|
|
soil moisture measurements (year started) |
2001 |
|
general description of soil moisture (dry, moist, wet,
saturated) |
dry and
moist |
|
soil texture: if non organic describe texture, if organic
indicate thickness of organic layer (cm) |
sandy |
|
SITE DESCRIPTION Small
hillock-hummocky northern taiga on sand and loam SOIL DESCRIPTION:
(predominant texture, i.e., ‘sand’, ‘gravel’,
‘peat’, etc.): Turbic
Cryosols (sandy) |
|
SAMPLING DESIGN AND METHOD:
1-ha grid consists of a square array
of surveyed permanent stakes separated by 10 m, yielding an 11 × 11 array
of sampling nodes on each grid. Thaw depth and snow sampling was conducted
twice by manual probing at each stake. The two values for each sampling point
are averaged, yielding a maximum of 121 data points per grid per probing date.
The active layer was not measured at locations where grid points intersect
rocks or deep water.
REFERENCES:
Fyodorov-Davydov,
D.G., Sorokovikov, V.A., Ostroumov, V.E., Kholodov,
A.L., Mitroshin, I.A., Mergelov, N.S., Davydov,
S.P., Zimov, S.A. & Davydova, A.I. 2004. Spatial and Temporal Observations of Seasonal Thaw in the
Northern Kolyma Lowland. Polar
Geography 28 (4): 308-325.