The variation and controls of mean transit times in Australian headwater catchments

Author:

Cartwright Ian1ORCID,Morgenstern Uwe2,Howcroft William3,Hofmann Harald4,Armit Robin1,Stewart Michael2ORCID,Burton Chad5,Irvine Dylan6ORCID

Affiliation:

1. School of Earth, Atmosphere and Environment Monash University Clayton Victoria Australia

2. GNS Science Lower Hutt New Zealand

3. Faculty of Science Engineering & Built Environment Deakin University Waurn Ponds Victoria Australia

4. School of Civil Engineering University of Queensland St Lucia Queensland Australia

5. Digital Earth Geoscience Australia Symonston Australian Capital Territory Australia

6. College of Science & Engineering Flinders University Bedford Park South Australia Australia

Funder

Australian Research Council

National Centre for Groundwater Research and Training

Melbourne Water

Monash University

Publisher

Wiley

Subject

Water Science and Technology

Reference85 articles.

1. The Role of Headwater Streams in Downstream Water Quality1

2. Land clearance and river salinisation in the western Murray Basin, Australia

3. Flow path depth is the main controller of mean base flow transit times in a mountainous catchment

4. Behrens H. Moser H. Oerter H. Rauert W. &Stichler W.(1979).Models for the runoff from a glaciated catchment area using measurements of environmental isotope contents. Isotope Hydrology 1978. Paper presented at Proceedings of the IAEA. Symposium in Neuherberg IAEA Vienna.

5. Linking water age and solute dynamics in streamflow at the H ubbard B rook E xperimental F orest, NH , USA

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