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Preliminary Comparison of Landscape Pattern–Normalized Difference Vegetation Index (NDVI) Relationships to Central Plains Stream Conditions

Jerry A. Griffith{dagger},*,a, Edward A. Martinkob, Jerry L. Whistlerc and Kevin P. Pricea

a Kansas Applied Remote Sensing Program and Dep. of Geography, Univ. of Kansas, Lawrence, KS 66045
b Kansas Applied Remote Sensing Program, Kansas Biological Survey and Dep. of Ecology and Evolutionary Biology, Univ. of Kansas, Lawrence, KS 66045
c Kansas Applied Remote Sensing Program, Univ. of Kansas, Lawrence, KS 66045



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Fig. 1. Watersheds used in the study.

 


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Fig. 2. Land use–land cover proportions in the watersheds stratified by ecoregion and/or size that are discussed in this study. WP, Western High Plains and Tablelands; FH, Flint Hills; GP, Glaciated Plains; SH, Nebraska Sand Hills; WCB, Western Corn Belt Plains; CIP, Central Irregular Plains; OH, Ozark Highlands; CGP, Central Great Plains; MRL, Mississippi River Lowlands. The proportions for some do not add to precisely 100% in some cases because not all of the possible eight land use–land cover types are shown.

 


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Fig. 3. Graphs of landscape measures for the five watersheds in the Western Corn Belt Plains (watersheds > 25 km2) with the highest habitat index (HI) scores and the five lowest. The graph shows what at first appear to be counterintuitive relationships: Watersheds with more agriculture, a landscape in which cover types are more aggregated, and less forest have better habitat conditions and lower turbidity. Turbidity is measured in nephelometric turbidity units (NTUs) and contagion is measured in percent with higher values indicating a more clumped or aggregated land cover.

 


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Fig. 4. Graphs of landscape measures for the five watersheds in the Western Corn Belt Plains (watersheds > 25 km2) with the highest habitat index (HI) scores and the five lowest. ED, edge density ([m/ha]/10); TP, total phosphorus (mg/L); SHDI, Shannon diversity index, ranging from 0 to 1 with higher values indicting a watershed with a relatively greater balance of land use–land cover (LULC) types; HI, habitat index ranging from 0 to 1 with higher scores indicating higher quality habitat; HI-a, riparian vegetation quality; HI-b, lack of disturbance in riparian zone; HI-c, substrate quality. This graph shows what at first appears to be counterintuitive relationships: Watersheds with higher quality habitat have a lower edge density and lower landscape diversity. In a rural, predominantly agricultural area, edge density might intuitively indicate more forest and hence lower turbidity and better substrate, and a higher Shannon diversity index might intuitively indicate more forest or grassland. But urban areas also add edge, and the presence of forest might be indicative of erosion from bluffs along the Missouri River. The correlation tables (Tables 5 and 6) indicate that, in fact, higher turbidity is associated with percent forest and percent urban.

 





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