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APPLICATIONOF GEO-SPATIALTECHNOLOGYFORTHE
ANALYSISOFRELIEFASPECTSOFTHESAPTLINGIBASIN
DR. SARDAR PATIL
Devrukh Shikshan Prasarak Mandal's
Nya. Tatyasaheb Athalye Arts, Ved. S.R. Sapre Commerce
and Vid. Dadasaheb Pitre Science College, Devrukh-415 804
Dist – Ratangiri ( Maharashtra State)
EMAIL: sardarpatilasp@gmail.com
Mob: 9096229741
Overview
• Morphometric analysis of a watershed
provides a quantitative description of the
drainage system (Strahler)
• The future progress of society and sustainable
development require a very good and detailed
knowledge of the physical environment
• The study of physical aspects of the earth
surface is the core of the spatial science
(Singh, Savindra, 1998), like Geography.
Overview
• The development in the field of Geo-Spatial
Technology (GST)
• The relief aspects of the drainage basins are
related to the study of three-dimensional
feature of the basin morphometry
• The study of relief aspects of drainage
morphometry is most useful in watershed
management and for the micro level planning.
THESTUDYREGION
OBJECTIVES
The main objective of the present research work is to
use the Geo-Spatial technology for the analysis of the
Relief aspects of the Basin Morphometry in the study
region. However, the specific objectives are as given
below.
– To analyze the Hypsometry of the Saptlingi Basin.
– To find out the clinographic pattern of the study region.
– To study gradient of the study region.
– To explain the relative relief of the study region.
METHODS OF DATA COLLECTION
• Primary data
• The Advanced Space-borne Thermal
Emission and Reflection Radiometer
(ASTER) Global Digital Elevation
Model (GDEM) remotely sensed data
• GARMIN'S Oregon 550 GPS
METHODS OF DATA ANALYSIS
• Geo-referenced in Arc GIS 9.3
• Watershed generation tool-Global Mapper
• Generate Contours Tool- Global Mapper
• Spatial Analyst Tool-Hydrology tool
• Clinographic analysis in Global Mapper
• DEM
RESULTS AND DISCUSSION
• The relief aspect includes the analysis of the
relation between area and altitude
• It also include clinographic analysis, analysis of
average ground slope, relative reliefs, relief
ratio, dissection index, profile of terrains and
the rivers etc.
• Most useful in the Integrated Watershed
Management (IWM) and sustainable
development
HYPSOMETRIC ANALYSIS
HI =
Mean Elevation- Minimum Elevation
Maximum Elevation- Minimum Elevation
Based on above equation the
Hypsometry Index of the study
region is 0.5.
Satara Presentation on applications of geospatial techniques
Satara Presentation on applications of geospatial techniques
CLINOGRAPHIC ANALYSIS
• Clinographic curves represent average slopes
between successive contours and thus present
panoramic view of the terrain.
CLINOGRAPHIC ANALYSIS
A B
C D
CLINOGRAPHIC ANALYSIS
E
SLOPE
Relative Reliefs
Relative relief =
Maximum relief
Basin perimeter
The study reveals that the
relative relief ratio of the
study region is 5.63.
CONCLUSION
• The study reveals that the Hypsometry Index
of the study region is 0.5.
• In the western part of the study region the
slope angle is less than 40 degree where as in
the eastern part it is more than 50 degree at
most of the sites.
• The relative relief ratio of the study region is
5.63.
Satara Presentation on applications of geospatial techniques

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Satara Presentation on applications of geospatial techniques

  • 1. APPLICATIONOF GEO-SPATIALTECHNOLOGYFORTHE ANALYSISOFRELIEFASPECTSOFTHESAPTLINGIBASIN DR. SARDAR PATIL Devrukh Shikshan Prasarak Mandal's Nya. Tatyasaheb Athalye Arts, Ved. S.R. Sapre Commerce and Vid. Dadasaheb Pitre Science College, Devrukh-415 804 Dist – Ratangiri ( Maharashtra State) EMAIL: sardarpatilasp@gmail.com Mob: 9096229741
  • 2. Overview • Morphometric analysis of a watershed provides a quantitative description of the drainage system (Strahler) • The future progress of society and sustainable development require a very good and detailed knowledge of the physical environment • The study of physical aspects of the earth surface is the core of the spatial science (Singh, Savindra, 1998), like Geography.
  • 3. Overview • The development in the field of Geo-Spatial Technology (GST) • The relief aspects of the drainage basins are related to the study of three-dimensional feature of the basin morphometry • The study of relief aspects of drainage morphometry is most useful in watershed management and for the micro level planning.
  • 5. OBJECTIVES The main objective of the present research work is to use the Geo-Spatial technology for the analysis of the Relief aspects of the Basin Morphometry in the study region. However, the specific objectives are as given below. – To analyze the Hypsometry of the Saptlingi Basin. – To find out the clinographic pattern of the study region. – To study gradient of the study region. – To explain the relative relief of the study region.
  • 6. METHODS OF DATA COLLECTION • Primary data • The Advanced Space-borne Thermal Emission and Reflection Radiometer (ASTER) Global Digital Elevation Model (GDEM) remotely sensed data • GARMIN'S Oregon 550 GPS
  • 7. METHODS OF DATA ANALYSIS • Geo-referenced in Arc GIS 9.3 • Watershed generation tool-Global Mapper • Generate Contours Tool- Global Mapper • Spatial Analyst Tool-Hydrology tool • Clinographic analysis in Global Mapper • DEM
  • 8. RESULTS AND DISCUSSION • The relief aspect includes the analysis of the relation between area and altitude • It also include clinographic analysis, analysis of average ground slope, relative reliefs, relief ratio, dissection index, profile of terrains and the rivers etc. • Most useful in the Integrated Watershed Management (IWM) and sustainable development
  • 9. HYPSOMETRIC ANALYSIS HI = Mean Elevation- Minimum Elevation Maximum Elevation- Minimum Elevation Based on above equation the Hypsometry Index of the study region is 0.5.
  • 12. CLINOGRAPHIC ANALYSIS • Clinographic curves represent average slopes between successive contours and thus present panoramic view of the terrain.
  • 15. SLOPE
  • 16. Relative Reliefs Relative relief = Maximum relief Basin perimeter The study reveals that the relative relief ratio of the study region is 5.63.
  • 17. CONCLUSION • The study reveals that the Hypsometry Index of the study region is 0.5. • In the western part of the study region the slope angle is less than 40 degree where as in the eastern part it is more than 50 degree at most of the sites. • The relative relief ratio of the study region is 5.63.