glacier monitoring in mongolia - global cryosphere watch · 2016. 2. 23. · glacier inventory,...
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Glacier monitoring in Mongolia G. Davaa
Research Institute of Meteorology, Hydrology and Environment, NAMEM, MEGDT,
Mongolia
Glaciers in the Altai Mts.
Objectives
1)Long term observation of representative glaciers to reveal
present condition of glaciers in Mongolia
Glaciers monitoring (mass balance, area, ice flow, thickness)
Climate monitoring
Hydrological monitoring
Reconstruction of past historical data
Collection of basic data for glacier model
2) To make an assessment for future changes of water
resources to take an adaptation measures
Modeling (climate, glacier, river flow and ecosystems)
Climate change and adaptation options (IWRM plans)
Indroduction
Potanin’s expeditions to northwestern Mongolia (1877-1879),
Rutkowski and Slowanski (1970): They made general,
descriptions of separate glaciers in the immediate vicinity of the
expedition’s routes.
First assessment on Mongolian glaciers made by Dashdeleg
et al. (1983) based on topographic map scaled as 1:100000 for
delineation of glaciers and estimated volume of glaciers using
Erasov’s equation.
Nikitin et al., 2001, Narozhny et al., 2006: There are long-
term mass balance records (WGMS) and also ice thickness of
glaciers was measured and estimated glacier volume dynamics
in the Russian Altai.
Permanent glacier monitoring has started in Mongolia, in
2003.
Detailed delineation of glaciers in the Turgen-Kharkhiraa
Mountain ranges made (Khrutsky and Golubeva, 2007) using
topographic map and Landsat images.
US–Mongolian expedition retraced and made analyses of field
data, repeated photographs from 1910 and 2010, topographic
maps from 1970, and satellite imagery from 1992 and 2010
were used to describe the changes in the glacial system. From
1910 to 2010, West Turgen Glacier receded by 600 m and
down-wasted by 70 m (Kamp et.al, 2013).
Kadota and Davaa (2007) reported glacier variations in
Mongolian Altai for 1950s-2000, which showed similar tendency
to those in Russian Altai in regard to types of glaciers, although
the magnitudes of the variations were different.
Glacier area estimated, using topographic map in 1940th and
LANDSAT data collected in 1990, 2002, 2006, 2011, 2015 by
Institute of Meteorology, Hydrology and Environment, Mongolia.
Indroduction
Konya et al. (2010) reported meteorological and ablation
features on a glacier in Mongolian Altay.
Herren et al. (2013) reported results of ice core from the
Tsambagarav Mts. and reconstruction of past climate for 6000
years.
Besides newly introduced glacier monitoring system (mass
balance, glacier thickness, ice flow velocity, terminus line shift,
climate in mountainous region, river flow), long-term
meteorological and hydrological data of stations, located in
valleys of glacier mountains are used for reconstruction of
climate and river flow data of glacier mountains and rivers,
draining from there.
Glacier Mountains in Mongolia
Glacier massive
are distributed
in 42 Mountains
in the country.
2010 data: There are Large glacier massive > 100 sq.km area is 1; Big massive (50-100 sq.km) is 1, Bigger (20-50 sq.km) are 3, Moderately big (10-20 sq.km) are 3, Medium (5-10 sq.km) are 5, Moderately small (3-5 sq.km) are 8, Small (1-3 ам кsq.km) are 15, Very small < 1 sq.km are 6.
Glacier Mountains in the Mongolian Altai
There are distributed about 600 glaciers in these 42 mountain massive.
Have been established 5 glacier monitoring stations, distributed along
the extension of Mongolian Altai range.
R U S S I A N F E D E R A T I O N
C H I N A
M O N G O L I A
Munkh hairkhan Mts.
Turgen Mts.
Tsambagarav Mts.
Tavanbogd Mts.
Sutai Mts.
Current observations on glaciers: Tavanbogd Mts.
Observations 2003-2015 (IMHE, Mongolia and JAMSTEC, Japan) at
the Tavanbogd glacier
・stake measurement, daily in June-Sep.
-mass balance
-flow (surface velocities) in Sept.
・Radio-echo soundings, 2 times made.
-ice thickness at the stakes
・Precipitation measurement at BC in June-Sept.
・Meteorological observation near the glacier, 2007-2015
Campbell, 1 hour, 3560 m
Hobo, 2 hours, 3091m, 2014-2015
Observation at Tsambagarav ice cap glacier
Observations 2004-2015 by IMHE at the Tsambagarav
glacier (Flat top glacier)
・stake measurement on lower/middle and top of the
glacier in June-Sept.
・Radio-echo soundings, 2 times made
-ice thickness at the stakes
• Hydrological station at the Ulaan-Am stream-
•Meteorological data collection with AWS – 2004-2015
AANDERAA, Campbell-1, Campbell-2, 1 hour, 30 min.
3654 m and Campbell- 2015, 2804 m
Wind speed and direction Air temperature Humidity Solar radiation Rainfall
Observation at Munkhhairkhan corrie glacier
Observations 2006-2015 by IMHE at the
Munkhhairkhan glacier (Corrie glacier)
• Hydrological station at the Doloon nuur streams –
2008-2015
•Meteorological data collection- AWS-2008-2015,
Campbell till 2013, HOBO since 2014, 2 hours, 3584 m
Hydrological stations
Wind speed and direction Air temperature Humidity Solar radiation Rainfall
Monitoring program: IMHE, 2005-2006, stationary monitoring since 2013-2015
• Glacier mass balance (JJAS) • Meteorology (AWS), Campbell, 1 hour, at 2858 м • River hydrology (Turgen) below the glacier –newly established hydrogauge with WL
sensor • Permafrost (3 boreholes)
Observation at Turgen valley glacier
Monitoring program: IMHE, Stationary monitoring since 2015 • Glacier mass balance (June and Sept.) • Meteorology (AWS), Campbell, 1 hour, at 2858 м • River hydrology (Zuil at Tonkhil) since 2004
Observation at Sutai ice cap glacier
Permafrost monitoring in Mongolia
Permafrost monitoring network in Mongolia
There are over 100 permafrost monitoring boreholes, belonging to several institutions and established in different periods of time.
Institutions Number of boreholes
IG 23 +13
IRIMHE 30
JAMSTEC 10
SHAR 32
Source: Ya.Jambaljav, IG, 2014
PERMAFROST Decadal changes in permafrost temperatures and depth
of seasonal freezing/thawing are indicators of changes
of climate in high latitude and mountain regions.
Mts region Hentei Hangai Hovsgol
Borehole
No Baganuur Argalant Terkh Chuluut Sharga Tsagaan nuur
Elevation,
m asl 1350 1385 2075 1870 1864 1547
Land form Plain of
depression
Small valley
bottom
High flood
plain
Top of the
pingo
Wide valley
bottom
Lake
depression
Ground Sandstone Loam Gravelly sand Ice and clay Gravelly sand Silt and clay
Ice content Low Medium Medium High Medium High
Measured
years 1976 2006 1988 2006 1969 2006 1969 2006 1968 2006 1989 2006
MAPT at
10 m -0.50 -0.09 -0.40 -0.24 -1.96 -1.49 -1.12 -0.80 -2.35 -1.63 -3.91 -3.37
Trend of
MAPT, oC/year
0.013 0.013 0.009 0.009 0.015 0.015 0.011 0.011 0.019 0.019 0.032 0.032
0.01-0.02 0.02-0.03
Source: N.Sharkhuu, 2008, Proceedings of 9th International Conference on Permafrost, Fairbank, Alaska
Glacier monitoring results
Reconstructed air temperature time series allow to estimate that annual average air temperature
increased by 1.0, 1.3, 1.1 and JJA average temperature has increased by 1.7-1.8 оС for the
period of 1940-2011 at the Tavanbogd, Tsambagarav and Mukhhairkhan Mts., respectively, оС.
Glacier inventory, area estimated, using topographic map compiled in 1940th and LANDSAT
data collected in 1990, 2002, 2006, 2011, 2015 by Institute of Meteorology, Hydrology and
Environment, Mongolia and glacier area has decreased by 29.9 % in last 70 years.
Ice thickness have been measured at selected glaciers in Mongolia and obtained equation as
glacier volume vrs. area was compared with the equation obtained by Nikitin S., and others,
2000, Narojny U., and Nikitin S., 2003, 2006 in Russian Altai and with the equation obtained
by Wang Zongtai ба Zhu Guocai, 2007 in China.
Water resources in glaciers in Mongolia has been re-estimated, it totals 19.4 cub. km in 2000.
Measured mass balance, flow velocity, terminus line and surface elevation changes and
featured changes in glaciers elements (Moulin, streams, moraine, crevasses, cave, bridge, ice
table).
Have been started climate modeling and simulation of past climate and glacier mass balance
and runoff modeling of rivers and streams draining from glaciers and climate change impact
assessment.
Conclusion
From the results of this study can be drawn following
conclusion:
Glaciers of Mongolian Altay have experienced a negative
mass balance in last decades and glacier area degreased and
small glaciers are disappearing.
The recent trends of abrubt warming in selected glaciers
under survey will be leading to negative state of mass balance.
Therefore, more comprehensive studies focused to climate
change impact assessment and adaptive measures in the frame
work of Integrated River basin management are highly
challenged.