Runoff generation mechanisms

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Results and DiscussionSpatial and Temporal Distribution and ConnectivityRainfall (mm/hr)6050403020100Discharge( m 3 /m in)4.0E-023.5E-023.0E-022.5E-022.0E-021.5E-021.0E-025.0E-030.0E+0010401050110011101120113011401150120012101220123012401250104010501100111011201130114011501200121012201230Time (hh:mm)Time (hh:mm)73% of the total areawas contributingsurface runoff41% of the total areawas contributingsurface runoff
Results and DiscussionSpatial and Temporal Distribution and ConnectivitySen, S., P. Srivastava, K. Yoo, J. Dane, J. Shaw, and M.S. Kang. 2008. SPATIAL AND TEMPORAL DYNAMICS ANDCONNECTIVITY OF RUNOFF CONTRIBUTING AREAS IN PASTURES OF THE SANDMOUNTAIN REGION OFALABAMA – A FIELD INVESTIGATION. Hydrological Processes (In preparation)
Page 1 and 2: Hillslope Hydrology of Alabama’sS
Page 3 and 4: Justification• Alabama ranks in t
Page 5 and 6: Runoff Generation ProcessesInfiltra
Page 7 and 8: Runoff Generation Processes• Fact
Page 9 and 10: • A pasture hillslope of 0.12 haw
Page 11 and 12: Surface Runoff Sensor• Surface se
Page 13 and 14: Instrumentation
Page 15 and 16: Results and DiscussionRunoff Genera
Page 23: Results and DiscussionSpatial and T
Page 27 and 28: Implications and Future Work• Sin

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