✦ LIBER ✦

Hydrologic Response to land use changes on the catchment scale

✍ Scribed by N. Fohrer; S. Haverkamp; K. Eckhardt; H.-G. Frede

Book ID: 114402482
Publisher: Elsevier Science
Year: 2001
Tongue: English
Weight: 700 KB
Volume: 26
Category: Article
ISSN: 1464-1909
DOI: 10.1016/s1464-1909(01)00052-1

No coin nor oath required. For personal study only.

📜 SIMILAR VOLUMES

Land use change and hydrological respons

Land use change and hydrological response in the Camel catchment, Cornwall

✍ A Sullivan; J.L Ternan; A.G Williams 📂 Article 📅 2004 🏛 Elsevier Science 🌐 English ⚖ 851 KB

Effects of land-use changes on the hydro

Effects of land-use changes on the hydrologic response of reclamation systems

✍ Giorgio Camorani; Attilio Castellarin; Armando Brath 📂 Article 📅 2005 🏛 Elsevier Science 🌐 English ⚖ 654 KB

Land-use impacts on storm-runoff generat

Land-use impacts on storm-runoff generation: scenarios of land-use change and simulation of hydrological response in a meso-scale catchment in SW-Germany

✍ Daniel Niehoff; Uta Fritsch; Axel Bronstert 📂 Article 📅 2002 🏛 Elsevier Science 🌐 English ⚖ 1011 KB

The impact of land use change on catchme

The impact of land use change on catchment hydrology in large catchments: The Comet River, Central Queensland, Australia

✍ L. Siriwardena; B.L. Finlayson; T.A. McMahon 📂 Article 📅 2006 🏛 Elsevier Science 🌐 English ⚖ 502 KB

The hydrological response of catchments

The hydrological response of catchments to simulated changes in climate

✍ Neil R. Viney; Murugesu Sivapalan 📂 Article 📅 1996 🏛 Elsevier Science 🌐 English ⚖ 371 KB

Effects of land-cover changes on the hyd

Effects of land-cover changes on the hydrological response of interior Columbia River basin forested catchments

✍ James R. VanShaar; Ingjerd Haddeland; Dennis P. Lettenmaier 📂 Article 📅 2002 🏛 John Wiley and Sons 🌐 English ⚖ 758 KB

## Abstract The topographically explicit distributed hydrology–soil–vegetation model (DHSVM) is used to simulate hydrological effects of changes in land cover for four catchments, ranging from 27 to 1033 km^2^, within the Columbia River basin. Surface fluxes (stream flow and evapotranspiration) and