Impact of Model Physics on Retrieving Soil Moisture and Soil Temperature
Soil airflow is crucial in determining surface evaporation, which subsequently affects the atmospheric modeling. However, most land surface models (LSMs) usually ignore the airflow and only employ the diffusion-based soil water and heat transport model. I
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Aims and Scope The series ‘‘Springer Theses’’ brings together a selection of the very best Ph.D. these from around the world and across the physical sciences. Nominated and endorsed by two recognized specialists, each published volume has been selected for its scientific excellence and the high impact of its contents for the pertinent field of research. For greater accessibility to non-specialists, the published versions include an extended introduction, as well as a foreword by the student’s supervisor explaining the special relevance of the work for the field. As a whole, the series will provide a valuable resource both for newcomers to the research fields described, and for other scientists seeking detailed background information on special questions. Finally, it provides an accredited documentation of the valuable contributions made by today’s younger generation of scientists.
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Yijian Zeng
Coupled Dynamics in Soil Experimental and Numerical Studies of Energy, Momentum and Mass Transfer Doctoral Thesis accepted by University of Twente, The Netherlands
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Author Dr. Yijian Zeng Faculty of Geo-Information Science and Earth Observation Water Resource Department University of Twente Enschede The Netherlands
ISSN 2190-5053 ISBN 978-3-642-34072-7 DOI 10.1007/978-3-642-34073-4
Supervisor Prof. Z. Su Faculty of Geo-Information Science and Earth Observation Water Resource Department University of Twente Enschede The Netherlands
ISSN 2190-5061 (electronic) ISBN 978-3-642-34073-4 (eBook)
Springer Heidelberg New York Dordrecht London Library of Congress Control Number: 2012951137 © Springer-Verlag Berlin Heidelberg 2013 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or here
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