Comparison of practices

Other: Remote monitoring

• Use of water resources
• Use of land resources
• Environmental protection

Country: Turkmenistan

Country: Kyrgyzstan

Province: Issyk Kul Region

District: Ak-Suu District

17,238 ha of barkhan (sand dune), takyr (dry-type playa) and solonchak (moist-type playa) sites of the Kara Kum Desert; deep ground water occurrence

Enilchek is a dendrite-type glacier originating around Khan Tengri Peak (6,995 m) with its tongue (43.2 km long and on average 2.2 km wide) descending to 2,800 m ASL.  Northern Enilchek Glacier is 38.2 km long (181.2 sq.km) and Southern Enilchek Glacier is 58.9 km long (567.2 sq.km).

Lake Merzbacher:

• 3,304 m ASL;
• volume – 0.12-0.25 km³;
• deepest point -- 75 m;
• average depth -- 35 m;
• water-surface lake area – 4.5 sq.km.

Lake Merzbacher formed at the end of the Small Ice Age (19^th century).  It has two pools called Upper and Lower Lakes divided by 400 m of elevation and 3-4 km long ice river with the same name.  In its southern part, the lower and larger part of the lake is limited by the glacial “dam”.  Every year (twice a year, in summer and winter periods) the lake’s lower part breaks into the Enilchek River Valley completely losing its water (discharge speed may exceed 1,000 m³/s) and dumping it in the course of 2-7 days via subglacial canals.  At the time of lake outburst, it accumulates 0.06-0.07 km³ of water.  Based on research data, lake bursts occur when water temperature in the lake rises to 10-15° Celsius.

Start date: 01.01.2012

End date: 31.12.2016

Start date: 01.01.2012

End date: 31.12.2013

Desertification and decreased productivity of desert pastures due to over-grazing around existing cattle watering sites

Lake Merzbacher’s outbursts often destroy bridges, roads and other engineering facilities/installations located along the rivers originating in the lake down to the Ak-Suu River on the territory of China.

Technology of building sardobas (stone-dome covered water collection and storage reservoirs) to enhance pasture water supply

1. Upgrading control and management systems;
2. Remote monitoring

Main actions:

• mudflow and flood risk assessment and surveying local population regarding sardobas’ locations.

Actions:

• selection of takyrs to construct sardobas jointly with local cattle-farmers;
• construction of sardobas jointly with local cattle-farmers;
• cleaning takyr surfaces.

Results:

• pastures that were not previously utilized due to absence of water sources returned to pasture rotation;
• pastures destroyed due to over-grazing started to restore;
• increased herd productivity due to reduced passage distances and higher fodder value of pastures.

The Sary-Dzhaz River Basin which includes Enilchek -- the largest glacier in the country – is one of main sources of fresh water and a potential source for hydropower in the region.

The region is of special significance as to investigating the probability of both natural and natural-technogenic disasters.  It also plays an important role in rational water supply in Kyrgyzstan and the adjacent territory of Xinjiang Autonomous Region of China, as well as planning large-scale infrastructure projects (ex.: cascading hydro-power stations).

Based on the observation data of the last decade, climate change is the reason behind the regressing Tien Shan glaciation.  It leads to reduction of shared water resources, activation of mud flows, floods and glacial lake outbursts.  The largest known glacier-dammed Lake Merzbacher is characterized by one of the most severe and regular annual disruptive glacial floods.  It was necessary to examine hydrological, climatic and glacial changes associated with altering region- and global-scale atmospheric circulations, i.e. their effect on the central section of Enilchek Glacier (confluence point of its two branches -- Northern and Southern Enilchek).

Actions:

Enilchek Glacier research was carried out on the premises of Merzbacher Station established jointly by CAIAG and GFZ in August 2009.  Subsequently, it is planned to expand the set of measuring tools used for studying Enilchek Glacier.

Project scope included field research in the Sary-Dzhaz and Enilchek River Basins, collection of measurements from automatic meteo- and seismic stations, hydro-posts on Northern Enilchek Bridge and Southern Enilchek ablation stake.

Automatic meteorological stations provide data on temperature, precipitation, humidity, atmospheric pressure, wind and total solar radiation necessary to reveal the impact of altering climatic parameters on glacier balance, discharge of the Enilchek River and outburst discharge regime of Lake Merzbacher.  Project efforts allowed better identification of summer glacial discharge for separate glaciers (Northern and Southern Enilchek) via automatic hydro-posts.

Water level and ice surface fluctuations in Lake Merz-bacher were subject to monitoring and registration via water pressure sensors developed GFZ, OpenGPS Sensor (laser scanning technology) and visual observations (high-resolution web-cameras).

Results:

The CAIAG monitoring network was established under research grants and third-party project investments.  The installed GPRS-modems allowed to automatically transfer data to CAIAG server on a daily basis.

The network of interlinked stations was created already under the GCO-CA Project, including MRZ1 and MRZ2 stations close to Lake Merzbacher on northern and southern walls of Northern and Southern Enilchek Glaciers.  The third ICED Station – to measure glacier speed and monitor the dam -- was installed on the ice dam.

The project allowed the e-mapping of the Sary-Dzhaz River Basin, making and assessing Enilchek Glacier geophysical and capacity measurements, as well as identifying lineaments, breaks and crossbars near outburst-prone Lake Merzbacher.  Analyses of satellite imagery allowed identifying rock slides in the form of paleoseismic dislocations within the 50 km radius of the merger point of the Sary-Dzhaz River and the Enilchek River (its left-bank tributary).  The deciphered paleoseismic dislocations prove the region’s high seismicity.  In the future, project results can be used for designing and building the Sary-Dzhaz Hydropower Station.

Financial and economic:

The received results manifest an important contribution to planning and implementing secure economic development efforts in the Sary-Dzhaz River Basin, in particular, designing, building and operating hydropower plants in the region.

Environmental:

Project outcomes serve basis for assessing and forecasting climatic and ecological variability of water resources.

Social:

• reduced probability of sudden destruction of engineering facilities;
• increased security for the residents of the Sary-Dzhaz River Basin.

Lessons learnt:

Construction of sardobas in takyr areas allows enhancing pasture water supply, thus, leading to the restoration of over-grazed pastures.

Recommendations:

The practice requires long-term planning and an integrated response with the early-on engagement of desertification experts (designing a set of measures to protect takyrs from sand drifts), state agencies (technical assistance) and pasture users (observance of pasture rotation schemes, prevention of takyrs from contamination and pollution).

Lessons learnt:

Research and monitoring of Southern and Northern Enil-chek Glaciers and Lake Merzbacher are of paramount importance due to the prospects of developing water, hydropower and mineral resources in the target basin.

Recommendations:

Long-term monitoring of glaciers and lakes is necessary to prevent the devastating outbursts of high-altitude lakes.

Traditional tools transferred from generation to generation that proved their efficiency in modern conditions

Foreign tools (transfer of foreign experience)

1. Cost of implementation: Low

2. Approximate cost of investment per 1 ha: $1,000-5,000

3. O&M costs: Low

4. Expert support: Needed at implementation stage

1. Cost of implementation: High

2. Approximate cost of investment per 1 ha:

3. O&M costs: High

4. Expert support: Not needed

Project title: Responding to climate change risks for dekhan farming system of Turkmenistan on national and local levels.

Project duration: 2012-2016. 

Project goal and objectives: build the adaptation capacity to respond to climate change impacts, including variability on local and national levels. 

Project beneficiaries: Bori Settlement (over 1,100 people) and Bo-Kurdak Settlement (about 4,500 people).

Project implementer: Ministry of Nature Conservation and UNDP

Project title: Examination of Enilchek Glacier to determine its balance, morphological and dynamic characteristics, and climatic and hydrological conditions.

Project duration: 2012-2013.

Project goal and objectives: measure a series of parameters necessary for explanation, simulation and forecasting of glacial, water, and atmospheric sub-systems in terms of potential risks of geo-catastrophes and water resources changes.

Project long-term goals: forecast climate and water resources change trends in Kyrgyzstan and Central Asia.

Scale of implementation and project beneficiaries: populations of the Sary-Dzhaz River Basin of the Kyrgyz Republic and the river’s lower reaches on the territory of the People's Republic of China.

Project implementer: Central Asian Institute for Applied Geosciences (CAIAG).

tm.undp.org

1. Central Asian Institute for Applied Geosciences, 2012-2013 Research Program;
2. Magnetometer Survey of Southern and Northern Enilchek (Inylchek) Glaciers in the area of Lake Merzbacher;
3. Presentation about the work of the institute;
4. On the geo-risk monitoring system in Central Asia;

SIC ICWC

 SIC ICWC