Wossenu Abtew Lanscape Surface Dynamics (2)
[Pages:21]Land Surface Dynamics and Hydrologic Connectivity
The Sahel The Sahel
Photos from , Lusile17., & vega.isara.fr
Wossenu Abtew, Ph.D., P.E., D.WRE Principal Civil Engineer
Water and Environment Consulting LLC, Affiliate, FIU Assefa M. Melesse, Ph. D., P.E., D.WRE Professor & Graduate Program Director, FIU
2020 International Conference on the Nile and Grand Ethiopian Renaissance Dam: Science, Conflict Resolution and Cooperation
August 20-21, 2020
Topics
? Landscape degradation and desertification ? What is the link between landscape dynamics, energy and mass,
the hydrologic cycle ? The importance of wetlands, lakes, riverine, forests, green
spaces and landscape management and restoration
(Lake Tana Watershed Regreening Ethiopia's highlands: A new hope for Africa)
Ethiopia: Source:
Overgrazing and Deforestation in Ethiopia
3
Desertification and Landscape Change
The Sahara has Expanded by 10% since 1920
Source: FAO; desertification in Africa
Wind Erosion
Desertification
? Overgrazing ? Deforestation ? Wetland loss ? Soil loss by wind
and water erosion
The Evaporation Process
Water must be available Energy to detach water molecules Wind to carry out water molecules Atmosphere must have space to hold water molecule or release
Energy Balance H+E=R-G
Abtew, W and A. Melesse. 2015. Chapter 3: Landscape Impact on Regional Hydrology and Climate. In: Melesse A. and W. Abtew (eds.). Landscape Dynamics, Soil and Hydrological Processes in Varied Climates, Springer.
Energy and Mass of Water
Evaporation
One liter of water One kg of water
2.45 MJ of energy 2.45 MJ of energy
Condensation
Surface Temperature of Forest and Drained Meadow with Road as seen by Thermovision Camera
Sensible Heat + Latent Heat = R - G
Energy Balance H+E=R-G
Modified from: Eiseltova, M., J. Pokorny, P. Hesslerova and W. Ripl. 2012. Chapter 14: Evapotranspiration - A driving force in landscape sustainability. Irmak A (ed.) Evapotranspiration Remote Sensing and Modeling. InTech (open access book)
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