EXAMPLES OF GLIMS INSTALL
EXAMPLES OF GLIMS GENERATOR
EXAMPLES OF GLIMS SOFTWARE
EXAMPLES OF GLIMS SERIES
EXAMPLES OF GLIMS DOWNLOAD

The SRTM topographic model was used for the calculation of the curves ( вЂњSrtmgl1 n -ASA SRTM Version 3.0вЂќ 2020a).Дata on land ice can be obtained from the Global Land Ice Measurements from Space glacier database GLIMS ( GLIMS and NSIDC 2005, updated 2018). And to come to an informed conclusion, one has to take into account all land ice features, including their altitude.ДЇigure 2.5: Hypsographic curves of the upper Syr Darya and Amu Darya catchments. The role of glaciers in the annual distribution of runoff is thus more substantial in the case of the Amu Darya as compared to the Syr Darya. Figure 2.5 shows the basinsвЂ™ hypsographic curves.Д®ven if we take into account that in the case of the basins of Pyandzh and Vakhsh the snow line is on average located at the height of 4вЂ™600 m - 4вЂ™500 m and in case of the basins of Naryn and Kara Darya at 4вЂ™000 m - 3вЂ™900 m, 19% - 22% of the reservoirs of Pyandzh and Vakhsh is located above the snow line, and in case of reservoirs of Naryn and Kara Darya it is only 4% - 5%. In the first two reservoirs, the mountains exceeding 5вЂ™000 m occupy 6.2% of their area, and the mountains higher than 4вЂ™000 m - 42%, in case of reservoirs of the second two rivers, the mountains exceeding 5вЂ™000 m occupy less than 1% of their area and the ones with altitudes over 4вЂ™000 m - only 4%. More specifically, we compare the two main subcatchments of the Vakhsh and Pyandzh Rivers in the Amu Darya and the Naryn and Kara Darya catchments in the Syr Darya 3. For this, it is instructive to start to look at the condition of discharge formation in the Amu Darya and Syr Darya basins (see Figure 2.4). Topographic data is from ( вЂњSrtmgl1 n -ASA SRTM Version 3.0вЂќ 2020a).ДЇirst, we study the role of glacier melt. Basin outlets (red dots) are chosen to correspond to the confluence of the two main rivers for each catchment. Exercise on creating GIS layers for import to RS MinerveДЇigure 2.4: Map of the upper Syr Darya and Amu Darya catchments.9.3.3 Computing Mean Monthly Temperature Climatology from CHELSA v1.2.1 data.9.3.2 Bias Correcting CHELSA v1.2.1 Precipitation Data for Snow Undercatch.9.3.1 Cutting CHELSA v.1.2.1 to CA Domain.9.3 Appendix C: Processing Climate Data.RSM: Add comparator and load discharge measurements.RSM: Export simulation results to data base.RSM: Create HBV model and edit parameters.QGIS: Calculate the area upslope of a point.9.2.1 QGIS: Verify projection of layer and re-project layer.QGIS: Merge SRTM tiles to a single layer.QGIS: Import SRTM layers using the SRTM plugin.GQIS: Managing panels visibility in QGIS.

EXAMPLES OF GLIMS INSTALL

QGIS: Install and activate plugins in QGIS3.

QGIS: Change the projection of the QGIS project.

EXAMPLES OF GLIMS DOWNLOAD

EE: Download SRTM data for a selected region.

8 Operationalization of Models - Opportunities and Challenges.

7.5.4 Generating and Assessing Out-of-Sample Forecasts.

7.5.3 Assessing the Quality of Forecasts.

7.5.1 Benchmark: Current Operational Forecasting Models in the Hydrometeorological Agencies.

7.5 Investigating and Engineering Predictors.

7.2 Forecasting in the Central Asian Hydromets.

7.1 Forecasting Using Predictive Inference.

7 Discharge Forecasting with Predictive Inference.

6.7 Application: Investigating Climate Change Impacts.

6.5.1 HBV example: Simple model of the Nauvalisoy river catchment.

6.4.2 Loading GIS Data and Model Creation.

6.4.1 Examining and Understanding the GIS Data.

6.3 Recap: The general modeling process.

EXAMPLES OF GLIMS GENERATOR

5.4.2 Using a Weather Generator to Simulate Daily Future Climate.

EXAMPLES OF GLIMS SERIES

Monthly Climate Time Series for 2006 - 2100

5.3.2 ERA5 Download and Data Resampling with PBCORR CHELSA.

5.3.1 CHELSA V1.2.1 Data and Bias Correction.

5.2.6 Manually edit the GIS layers for import in RS MINERVE.

5 Data Retrieval, Preparation & Analysis.

4.4 Application to Central Asian River Basins.

4.3 Hydrological Response to a Changing Climate.

4.2 Effects of Snow Ratio on Annual Runoff within the Budyko Framework.

4.1 Derivation of the Budyko Relationship.

4 Budyko-Type Long-term Water Balance Modeling.

3.2.4 Discharge Estimation from the Ungauged Kosku Tributary.

2.1 Regional Hydro-Climatological Features.

1.2 Post-Transition Development and Challenges.

1.1 The Taming of the Central Asian Rivers.

1 Short History of Water in Central Asia.

Day 9: Student presentations and wrap-up of workshop.

Day 6: Model calibration and validation.

Day 3: Hydrological models & Introduction to RS Minerve.

Day 2: Hydrological processes & characterization.

EXAMPLES OF GLIMS SOFTWARE

Day 1: Introduction and installation of software.

Examples of glims