VZJ sign up for etocs
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 24 January 2007
Published in Vadose Zone J 6:77-92 (2007)
DOI: 10.2136/vzj2006.0001
© 2007 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Faybishenko, B.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Faybishenko, B.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Faybishenko, B.
Related Collections
Right arrow Global Change
Right arrow Water Flow Models
Right arrow Infiltration

ORIGINAL RESEARCH

Climatic Forecasting of Net Infiltration at Yucca Mountain Using Analogue Meteorological Data

Boris Faybishenko*

Earth Sciences Division, Lawrence Berkeley National Lab., Berkeley, CA 94720
* Corresponding author (bfayb{at}lbl.gov)

Received 6 January 2006.

At Yucca Mountain, NV, future changes in climatic conditions will probably alter net infiltration, drainage below the bottom of the evapotranspiration zone within the soil profile, or flow across the interface between soil and the densely welded part of the Tiva Canyon Tuff. The objectives of this study were to: (i) develop a semiempirical model and forecast average net infiltration rates, using the limited meteorological data from analog meteorological stations, for interglacial (present day), and future monsoon, glacial transition, and glacial climates over the Yucca Mountain region; and (ii) corroborate the computed net infiltration rates by comparing them with the empirically and numerically determined groundwater recharge and percolation rates through the unsaturated zone from published data. This study approached calculations of net infiltration, aridity, and precipitation-effectiveness indices using a modified Budyko's water-balance model, with reference-surface potential evapotranspiration determined from the radiation-based Penman formula. Results of calculations show that net infiltration rates are expected to generally increase from the present-day climate to monsoon climate, to glacial transition climate, and then to the glacial climate, following a power law relationship between net infiltration and precipitation. The forecasting results indicate the overlap between the ranges of net infiltration for different climates. Forecasting of net infiltration for different climate states is subject to numerous uncertainties associated with selecting climate analog sites, using relatively short analog meteorological records, neglecting the effects of vegetation and surface runoff and run-on on a local scale, as well as possible anthropogenically induced climate changes.

Abbreviations: DRI, Desert Research Institute • G, glacial • IG, interglacial • IM, intermediate or glacial transition • M, monsoon




This article has been cited by other articles:


Home page
Vadose Zone JHome page
S. Finsterle, C. Doughty, M.B. Kowalsky, G. J. Moridis, L. Pan, T. Xu, Y. Zhang, and K. Pruess
Advanced Vadose Zone Simulations Using TOUGH
Vadose Zone J., May 27, 2008; 7(2): 601 - 609.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2007 by the Soil Science Society of America.