Year |
Citation |
Score |
2010 |
White JD, Prochnow SJ, Filstrup CT, Scott JT, Byars BW, Zygo-Flynn L. A combined watershed-water quality modeling analysis of the Lake Waco reservoir: I. Calibration and confirmation of predicted water quality Lake and Reservoir Management. 26: 147-158. DOI: 10.1080/07438141.2010.495315 |
0.321 |
|
2008 |
Scott JT, Doyle RD, Prochnow SJ, White JD. Are watershed and lacustrine controls on planktonic N2 fixation hierarchically structured? Ecological Applications : a Publication of the Ecological Society of America. 18: 805-19. PMID 18488636 DOI: 10.1890/07-0105.1 |
0.341 |
|
2008 |
Prochnow SJ, White JD, Scott T, Filstrup CD. Multi-Scenario Simulation Analysis in prioritizing management options for an impacted watershed system Ecohydrology and Hydrobiology. 8: 3-15. DOI: 10.2478/V10104-009-0001-4 |
0.381 |
|
2007 |
Prochnow SJ, White JD, Scott T, Filstrup C. Small Reservoir Impact on Simulated Watershed-Scale Nutrient Yield Research Letters in Ecology. 2007: 1-4. DOI: 10.1155/2007/12571 |
0.414 |
|
2007 |
Duke JR, White JD, Prochnow SJ, Zygo L, Allen PM, Muttiah RS. The use of remote sensing and modelling to detect small-dam influences on land-use changes along downstream riparian zones Ecohydrology and Hydrobiology. 7: 23-25. DOI: 10.1016/S1642-3593(07)70186-6 |
0.427 |
|
2006 |
Prochnow SJ, Atchley SC, Boucher TE, Nordt LC, Hudec MR. The influence of salt withdrawal subsidence on palaeosol maturity and cyclic fluvial deposition in the Upper Triassic Chinle Formation: Castle Valley, Utah Sedimentology. 53: 1319-1345. DOI: 10.1111/J.1365-3091.2006.00821.X |
0.469 |
|
2006 |
Prochnow SJ, Nordt LC, Atchley SC, Hudec MR. Multi-proxy paleosol evidence for middle and late Triassic climate trends in eastern Utah Palaeogeography, Palaeoclimatology, Palaeoecology. 232: 53-72. DOI: 10.1016/J.Palaeo.2005.08.011 |
0.469 |
|
2005 |
Prochnow SJ. Triassic paleosol catenas associated with a salt-withdrawal minibasin in southeastern Utah, U.S.A. Rocky Mountain Geology. 40: 25-49. DOI: 10.2113/40.1.25 |
0.458 |
|
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