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Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

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Page 1: Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

Dr. Conrad HeatwoleCenter for Watershed Studies

Virginia Tech, Blacksburg

Page 2: Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

Study watersheds – Magodi

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#0Luelo

MphiriKamwamphula

Kanyanga

Stream gage Weather station Rain gage Manual raingage

Page 3: Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

Paired Forest/Ag. Watersheds

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131

Gate4

Khuyu school

Chazovu school

Kamwamphul

a

Luelo

ZAWA

gate

Forested watershed

Agricultural watershed

Page 4: Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

Cropland expansion 1989-2007

1989Landsat

Page 5: Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

Cropland expansion 1989-2007

2002Landsat

Page 6: Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

Cropland expansion 1989-2007

2007Ikonos

Page 7: Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

Cropland expansion 1989-2007

Cropland expansion 1989-2007 1989Landsat

Page 8: Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

Cropland expansion 1989-2007

1989Landsat

Polygons are cleared areason May 2007 EnsoMosaic

Page 9: Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

Slope map of area

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131130

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Manga

Emusa EDP

Kanga Depot

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Dambo watershe

dsPaired

watersheds

Slope (%)

Slope calculated from 30m elevation grid derived from SRTM data using cubic interpolation.

Page 10: Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

Relation of cleared areas to landscape position

Maps of elevation and slope with the Enso cleared areas overlayed

Page 11: Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

Relationship between slope and cleared areas Cleared areas (digitized from 2007

Enso/Mosaic aerial imagery as seen in above slides) are overlaid on the slope map. Slope data is classified in 1% increments.

Areas at different slope values are tabulated. Cumulative areas determined and graphed as a % of the area.

Page 12: Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

Comparing slopes of cleared land in hill and plateau regions

Graph of cumulative percent area less than a certain slope

Data is only for cleared area on the 2007 Enso/Mosaic

Example – at 4% slope:45% of hill area and 83% of

plateau area is less than 4% Conversely, 55% of hill area

is greater than 4% slope, but only 17% of the plateau area.

Cumulative distribution of cleared area based on slope

Page 13: Dr. Conrad Heatwole Center for Watershed Studies Virginia Tech, Blacksburg

Comparing slopes of cleared land for three watersheds

Observations: Kamwamphula is steeper than

Luelo; both are much steeper than the plateau area

While about 13% of the plateau watershed is greater than 4% slope, 45 to 60% of the hill area is

Cleared areas tend to the lower slopes, but surprisingly represent the range of slopes in the watershed.

cleared areas are not exclusively on the low slopes

The curves for the more fully cleared Luelo are closest, indicating that over time, cleared land represents the whole watershed – not just flatter areas

The curves for Kamwamphula are further apart, showing that initial clearing is on flatter areas. However, the trend seen in the Luelo is to be expected.

Cumulative distribution of area based on slope for a plateau

watershed and two watersheds in the hill region