Axel Bronstert 2005.Pdf

Total Page:16

File Type:pdf, Size:1020Kb

Axel Bronstert 2005.Pdf I Axel Bronstert Jesus Carrera Pavel Kabat Sabine Lütkemeier Coupled Models for the Hydrological Cycle Integrating Atmosphere, Biosphere, and Pedosphere III Axel Bronstert Jesus Carrera Pavel Kabat Sabine Lütkemeier (Editors) Coupled Models for the Hydrological Cycle Integrating Atmosphere, Biosphere, and Pedosphere With 92 Figures, 19 in colour and 20 Tables IV Preface Axel Bronstert Pavel Kabat University of Potsdam Wageningen University and Institute for Geoecology Research Centre Chair for Hydrology and Climatology ALTERRA Green World Research P.O. Box 60 15 53 Droevendaalsesteeg 3 14415 Potsdam 6708 PB Wageningen Germany The Netherlands Jesus Carrera Sabine Lütkemeier Technical University of Catalonia (UPC) Potsdam Institute for Department of Geotechnical Engineering Climate Impact Research and Geosciences Telegrafenberg School of Civil Engineering 14473 Potsdam Campus Nord, Edif. D-2 Germany 08034 Barcelona Spain Library of Congress Control Number: 2004108318 ISBN 3-540-22371-1 Springer Berlin Heidelberg New York This work is subject to copyright. All rights are reserved, whether the whole or part of the material is concerned, specifi cally the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfi lm or in any other way, and storage in data banks. Duplication of this publication or parts thereof is permitted only under the provisions of the German Copyright Law of September 9, 1965, in its current version, and permission for use must always be obtained from Springer. Violations are liable to prosecution under the German Copyright Law. Springer is a part of Springer Science+Business Media springeronline.com © Springer-Verlag Berlin Heidelberg 2005 Printed in Germany The use of general descriptive names, registered names, trademarks, etc. in this publication does not imply, even in the absence of a specifi c statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. Cover design: Erich Kirchner Production: Almas Schimmel Typesetting: PR-Graphix, Karl C. Stahl, Heidelberg Printing: Mercedes-Druck, Berlin Binding: Stein + Lehmann, Berlin Printed on acid-free paper 30/3141/as - 5 4 3 2 1 0 V Preface Freshwater resources are an indispensable part of all terrestrial ecosystems. The Dublin Statement on Water and Sustainable Development states: “Scarcity and misuse of fresh water pose a serious and growing threat to sustainable development and protection of the environment. Human health and welfare, food security, industrial development and the ecosystems on which they depend are at risk, unless water and land resources are managed more effectively in the present decade and beyond than they have been in the past“. Similarly, the fi rst principle defi ned at the Dublin Conference states “Fresh water is a fi nite and vulnerable resource, essential to sustain life, development and the environment“ (UNESCO 1996). Strategies for sustainable development must be based on an accurate assessment of the Earth‘s carrying capacity and resilience to human activity. A deeper understanding of the interconnections between water, nutrient and biogenic cycles, and the energy fl ows of land, oceans and atmos phere, is crucial (UNCED 1992). AGENDA 21 calls for an “Integrated Approach to Land- Resource Use, and Protecting and Managing Freshwater Resources“. Increasing demand for land – a fi nite resource – and for the natural resources land supports is creating competition and confl ict that results in land degradation. The Framework and General Outline of IHP-V (www.unesco.org/water/ ihp/) states that if future water resource develop ment and management schemes are to be sustainable, they will have to deal effectively with environmental and social consequences; land-water link ages; allocation of water among competing uses and users; and achieving effective imple mentation. To achieve these goals, four areas of concern need addressing: 1. the role of scales in hydrological processes; 2. vulnerability of the environ ment; 3. integrated water resource management; and 4. education, training and transfer of technologies. VI Preface IHP Project 1.2 addresses the fi rst two, in particular, fostering the development of coupled hydroecologi cal/atmospheric models, synthesising hydrological data relevant to the calibration of those models and identifying the effects of enhanced atmospheric carbon dioxide. However, it is important to keep the last two goals in mind in order to stimulate stronger interactions between research, education and application and to emphasise integrated resource management and science. The International Dialogue on Water and Climate (DWC) aims to improve interactions between climate scientists and the water resource management. DWC (www.waterandclimate.org) bridges the information gaps between the water and climate sectors to improve our capacity to cope with the impacts on water management of increasing climate variability and change. The goal of the Dialogue is to develop a knowledge base, generate widespread awareness, identify policy and management options that build such capacities, learn from the experiences throughout the world, and make this knowledge available to the most affected communities. In general, coupled models are developed in pursuit of a particular objective and will therefore always have bias towards particular processes and phenomena. Similarly, this document is deliberately biased to place greater emphasis on hydrological processes and less emphasis on processes elsewhere in the coupled system. Later, for instance, when the interrelationships between processes is explored, processes and phenomena in the hydrological system are diagnosed in greater detail than are atmospheric, land-cover and transport processes. Further, to focus more on land-surface hydrological/atmospheric coupling, the domain of interest considered is limited to coupling processes relevant at the spatial scale of regions or large catchments. It is assumed, therefore, that either the incoming and outgoing atmospheric fi elds around the continental domains are measured or, if they are calculated elsewhere in a global coupled model, that the coupling between oceans and the atmosphere has been represented adequately. When modelling the hydrological system, it is not always necessary that all (or indeed any) coupling processes be represented. There are, however, at least four general situations where the use of coupled models is essential, as follows. • It is not feasible or economic to measure the boundary between com- partments in the modelled hydro-geo-biosphere system and thereby isolate them. This will be common when models are being used in truly predictive mode. VII • Observations of two or more state variables that are coupled cannot be modelled simultaneously unless the processes that couple them are in- cluded in the model. Sometimes, for instance, this is the case for models that describe the fl ows not only of water quantity but also of the chemi- cal composition of that moving water simultaneously. Representing both with a coupled model can reveal hitherto unrecognised weaknesses in the uncoupled description of water fl ow. • The science that is being addressed is beyond the normal range of ac- tivity and interest of specialists in individual coupled processes. In this case, the discipline of developing a coupled model can often produce totally new scientifi c understanding that would not otherwise have been possible. • Vulnerability assessments of the whole system are undertaken. This book is intended primarily for applied scientists and graduate students. It should also become a valuable source of information for hydrology and water resource management professionals who wish to advance their knowledge of the key principles of the coupled climate- hydrology system, and to use water system management models. As such, this book will be a valuable help in education and training. Mike Bonell, Axel Bronstert, Pavel Kabat, Jim Shuttleworth Agenda 21 (1993) Programme of action for sustainable development. Rio declaration on environment and development. The fi nal text of agreements negotiated by governments at the United Nations Conference on Environment and Development (UNCED), 3 - 14 June 1992, Rio de Janeiro, Brazil. New York, NY: United Nations, p 294 UNCED (1992) Report of the United Nations Conference on Environment and Development: Rio de Janeiro, 3 - 14 June 1992, New York, United Nations publication VIII Preface Acknowledgements The Editors would like to express their sincere thanks to the International Hydrology Programme (IHP) of UNESCO, to the former Core Project of the International Geosphere-Biosphere Programme “Biospheric Aspects of the Hydrological Cycle (BAHC)” and to the Dialogue on Water and Climate (DWC). All these three international programmes helped in convening workshops for the authors or in providing funding to fi nalise the book for publication. We are grateful to the German Federal Ministry of Education and Research (BMBF) for fund ing the BAHC Project Offi ce at the Potsdam Institute for Climate Impact Research (PIK). The Dutch Ministry of Development Cooperation provided support through the DWC. Additional funding and support have been provided by the German IHP-HWRP (Hydrology and Water Resources Programme of the WMO) Committee. We also wish to thank Ursula Werner (PIK) for converting most of the fi gures and Andreas Bauer (University of Potsdam) for additional technical support. Cover design: River
Recommended publications
  • Climate Modelling Primer
    A Climate Modelling Primer A Climate Modelling Primer, Third Edition. K. McGuffie and A. Henderson-Sellers. © 2005 John Wiley & Sons, Ltd ISBN: 0-470-85750-1 (HB); 0-470-85751-X (PB) A Climate Modelling Primer THIRD EDITION Kendal McGuffie University of Technology, Sydney, Australia and Ann Henderson-Sellers ANSTO Environment, Australia Copyright © 2005 John Wiley & Sons Ltd, The Atrium, Southern Gate, Chichester, West Sussex PO19 8SQ, England Telephone (+44) 1243 779777 Email (for orders and customer service enquiries): [email protected] Visit our Home Page on www.wileyeurope.com or www.wiley.com All Rights Reserved. No part of this publication may be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, mechanical, photocopying, recording, scanning or otherwise, except under the terms of the Copyright, Designs and Patents Act 1988 or under the terms of a licence issued by the Copyright Licensing Agency Ltd, 90 Tottenham Court Road, London W1T 4LP, UK, without the permission in writing of the Publisher. Requests to the Publisher should be addressed to the Permissions Department, John Wiley & Sons Ltd, The Atrium, Southern Gate, Chichester, West Sussex PO19 8SQ, England, or emailed to [email protected], or faxed to (+44) 1243 770620. Designations used by companies to distinguish their products are often claimed as trademarks. All brand names and product names used in this book are trade names, service marks, trademarks or registered trademarks of their respective owners. The Publisher is not associated with any product or vendor mentioned in this book. This publication is designed to provide accurate and authoritative information in regard to the subject matter covered.
    [Show full text]
  • The Prophet of Climate Change James Lovelock Rolling Stone
    The Prophet of Climate Change: James Lovelock : Rolling Stone 4/14/10 6:53 AM Advertisement PRINTER FRIENDLY URL: http://www.rollingstone.com/politics/story/16956300/the_prophet_of_climate_change_james_lovelock Rollingstone.com Back to The Prophet of Climate Change: James Lovelock The Prophet of Climate Change: James Lovelock One of the most eminent scientists of our time says that global warming is irreversible — and that more than 6 billion people will perish by the end of the century JEFF GOODELL Posted Nov 01, 2007 2:20 PM ADVERTISEMENT At the age of eighty-eight, after four children and a long and respected career as one of the twentieth century's most influential scientists, James Lovelock has come to an unsettling conclusion: The human race is doomed. "I wish I could be more hopeful," he tells me one sunny morning as we walk through a park in Oslo, where he is giving a talk at a university. Lovelock is a small man, unfailingly polite, with white hair and round, owlish glasses. His step is jaunty, his mind lively, his manner anything but gloomy. In fact, the coming of the Four Horsemen -- war, famine, pestilence and death -- seems to perk him up. "It will be a dark time," Lovelock admits. "But for those who survive, I suspect it will be rather exciting." In Lovelock's view, the scale of the catastrophe that awaits us will soon become obvious. By 2020, droughts and other extreme weather will be commonplace. By 2040, the Sahara will be moving into Europe, and Berlin will be as hot as Baghdad.
    [Show full text]
  • The Dynamic Response of the Global Atmosphere-Vegetation Coupled System
    THE UNIVERSITY OF READING Department of Meteorology The Dynamic Response of the Global Atmosphere-Vegetation coupled system John K. Hughes A thesis submitted for the degree of Doctor of Philosophy October 2003 ’Declaration I confirm that this is my own work and the use of all material from other sources has been properly and fully acknowledged’ John Hughes The Dynamic Response of the Atmosphere-Vegetation coupled system Abstract Concern about future changes in the carbon cycle have highlighted the importance of a dy- namic representation of the carbon cycle in models, yet this has not been fully assessed. In this thesis, we investigate the dynamic carbon cycle model included within the Hadley Centre’s model. In order to understand the behaviour of the vegetation model a simplified model, describing the behaviour of a single plant functional type is derived. The ability of the simplified model to simulate vegetation dynamics is validated against the behaviour of the full complexity model. The dynamical properties of the simplified model are then investigated. To further investigate the dynamic response of vegetation, a 300 year climate model simulation of terrestrial vegetation re-growth from global desert has been performed. Vegetation is shown to introduce large time lags in land surface properties. This large memory in the terrestrial carbon cycle is an important result for GCM simulations. The large timescale also affects the response of existing vegetation to climatic forcings. The behaviour of the land surface in terms of source-sink transitions of atmospheric CO2 is discussed. It is found that the transitions between source and sink of CO2 are dependant on the vegetation timescales.
    [Show full text]
  • Chaos Theory and Its Application in the Atmosphere
    Chaos Theory and its Application in the Atmosphere by XubinZeng Department of Atmospheric Science Colorado State University Fort Collins, Colorado Roger A. Pielke, P.I. NSF Grant #ATM-8915265 CHAOS THEORY AND ITS APPLICATION IN THE ATMOSPHERE Xubin Zeng Department of Atmospheric Science CoJorado State University Fort Collins, Colorado Summer, 1992 Atmospheric Science Paper No. 504 \llIlll~lIl1ll~I""I1~II~'I\1 U16400 7029194 ABSTRACT CHAOS THEORY AND ITS APPLICATION IN THE ATMOSPHERE Chaos theory is thoroughly reviewed, which includes the bifurcation and routes to tur­ bulence, and the characterization of chaos such as dimension, Lyapunov exponent, and Kolmogorov-Sinai entropy. A new method is developed to compute Lyapunov exponents from limited experimental data. Our method is tested on a variety of known model systems, and it is found that our algorithm can be used to obtain a reasonable Lyapunov­ exponent spectrum from only 5000 data points with a precision of 10-1 or 10-2 in 3- or 4-dimensional phase space, or 10,000 data points in 5-dimensional phase space. On 1:he basis of both the objective analyses of different methods for computing the Lyapunov exponents and our own experience, which is subjective, this is recommended as a good practical method for estiIpating the Lyapunov-exponent spectrum from short time series of low precision. The application of chaos is divided into three categories: observational data analysis, llew ideas or physical insights inspired by chaos, and numerical model output analysis. Corresponding with these categories, three subjects are studied. First, the fractal dimen­ sion, Lyapunov-exponent spectrum, Kolmogorov entropy, and predictability are evaluated from the observed time series of daily surface temperature and pressure over several regions of the United States and the North Atlantic Ocean with different climatic signal-to-noise ratios.
    [Show full text]
  • Interspecific Competition Affects Temperature Stability in Daisyworld
    T ellus (2000), 52B, 980–984 Copyright © Munksgaard, 2000 Printed in UK. All rights reserved TELLUS ISSN 0280–6509 Interspecific competition affects temperature stability in Daisyworld By JOEL E. COHEN1* and ALBERT D. RICH2, 1Rockefeller University and Columbia University, 1230 York Avenue, Box 20, New York, NY 10021-6399, USA; 2Rockefeller University, New York, and Soft Warehouse, Honolulu, USA (Manuscript received 12 February 1999; in final form 11 October 1999) ABSTRACT The model of Daisyworld showed that nonteleological mechanistic responses of life to the physical environment can stabilize an exogenously perturbed environment. In the model, 2 species of daisies, black and white, stabilize the global temperature of a planet exposed to different levels of insolation. In both species, the response of the growth rate to local temperature is identical, but differences in albedo between the 2 species generate differences in local temper- atures. The shifting balance between the daisies keeps the global temperature in a range suitable for life. Watson and Lovelock made the stronger claim that ‘‘the model always shows greater stability with daisies than it does without them.’’ We examined this claim by introducing an extra source of competition into the equations that describe the interactions between the daisy species. Depending on the parameters of competition, temperatures can vary more widely with increasing insolation in the presence of daisies than without them. It now seems possible, timely and perhaps necessary, to include an accurate representation of interspecific competition when taking account of vegetational influences on climate. 1. Introduction suitability of Earth for life (Lovelock, 1988; Lenton, 1998). To demonstrate that planetary It has long been recognized that life influences ‘‘homeostasis by and for the biosphere’’ could in physical and chemical environments and vice principle work by mechanisms that entailed no versa, at all scales from the local to the global teleology, Watson and Lovelock (1983) proposed (Lotka, 1925).
    [Show full text]
  • NATS 101, Sec 42 &
    GC170A-1 The Earth & Its Environment Lecture Sections 001+002 & 003+004 FALL 2011 INTRODUCTION TO GLOBAL CHANGE INSTRUCTOR: Dr. Katie Hirschboeck CLASS NOTES PACKET Fall 2011 HOW TO USE THIS CLASS NOTES PACKET Welcome to GC-170A-1! This CLASS NOTES packet is designed to be a companion to the classroom portion of GC-170A-1 Introduction to Global Change, taught by Dr. Katie Hirschboeck. You should bring this packet with you to every class. (You do NOT need to bring the textbooks: The Science of Global Change: An Introduction and Dire Predictions with you to class, unless announced in advance.) This packet contains the following: Selected notes with definitions, key points, & figures to accompany Dr. H’s lecture presentations on the course topics. Some fill-in-the-blank interactive sections that accompany a few of the lectures Several blank pages for entering your own outlines, notes, sketches and summaries as you review each topic after class while studying. Your own copy of handout materials used in class during many of the group activities, so you can take your own notes while working together as a group and refer to the activity later. More detailed background reading material that isn’t in your regular textbook to supplement some of the topics. Appendices that include items needed for specific activities and assignments at different points during the semester. Directions on how to find Dr. H’s office in the Laboratory of Tree-Ring Research (last page). See the GC-170A-1 WEBPAGE & D2L site for the latest versions of: Course Syllabus,
    [Show full text]
  • The Parable of Daisyworld: a Comprehensive Analysis
    THE PARABLE OF DAISYWORLD: A COMPREHENSIVE ANALYSIS PHILIP J. PLATTS Abstract. The Daisyworld model was conceived by Watson and Lovelock (1983), to provide insight into temperature regulation on Earth. The close coupling between non-intelligent lifeforms (two varieties of daisy) and their environment is shown to regulate the planet's temperature, across a wide range of solar luminosities. Attempting to model the Earth in all its grandeur would be an undertaking of unthinkable complexity. The simplifications required to keep Daisyworld accessible prompt us to study the model with caution. I take care to discuss the validity of each assumption that the authors make, before analysing the dynamical systems at work. I investigate how increasing the diversity of life affects the global temper- ature. This is, after all, the most striking difference between Daisyworld and planet Earth. I find that, the more species present, the more efficient the coupled system of biospere and geosphere becomes in its capacity to regulate Daisyworld's temperature. However, once Darwinian evolution is allowed, di- versity actually hinders the flowers' ability to survive large perturbations in their environment. Citation: Platts PJ (2003). The Parable of Daisyworld: A Comprehensive Anal- ysis. BSc Dissertation, University of York, UK Date: May 2003. 1 2 PHILIP J. PLATTS Contents 1. Introduction 2 2. Daisyworld 4 3. The Equations Explained 5 3.1. How the Flowers Grow 5 3.2. An Example: Emptyworld 7 3.3. Global Temperature 7 3.4. Local Temperature 8 3.5. Simplifying Local Temperature 9 3.6. Emptyworld Revisited 11 4. The Fixed Point at the Origin 11 4.1.
    [Show full text]
  • Uri J. Wilensky - 1
    Uri J. Wilensky - 1 URI J. WILENSKY Northwestern University 847-467-3818 (tel) Learning Sciences & Computer Science 847-491-8999 (fax) Center for Connected Learning & Computer-Based Modeling [email protected] Evanston, IL 60208 ACADEMIC WORK EXPERIENCE / EDUCATION Northwestern University, Evanston, IL Professor of Learning Sciences, Computer Science & Complex Systems 2008 – present Faculty member, program in Cognitive Science 2000 - present Faculty member, program in Technology and Social Behavior 2009 - present Faculty member, Segal Design Center Research Council 2014 – present Governing Board, Northwestern Institute on Complex Systems 2004 - present Associate Professor of Learning Sciences & Computer Science 2000 – 2008 Director of Center for Connected Learning & Computer-Based Modeling 2000 - present Shepard undergraduate residential college fellow 2007 - present Other University affiliations: University of Haifa Tufts University, Medford, MA 1994 - 2000 Associate Professor of Computer Science 1999 – 2000 Director of Center for Connected Learning 1994 - 2000 Assistant Professor of Education and Child Development 1994 - 1999 Director of Mathematics and Science Teacher Education Programs 1994 - 1999 Affiliated Faculty in Computer Science, Media and Communications, and Cognitive Science. Massachusetts Institute of Technology, Cambridge, MA 1998 - 1999 Post-doctoral Fellow 1993 - 1994 Mathematics Education, Learning Technologies Ph.D. in Media Arts and Sciences, 1993 1988-1993 Thesis: Connected Mathematics: Building Concrete Relationships
    [Show full text]
  • Collective Dynamics and Homeostatic Emergence in Complex Adaptive Ecosystem
    ECAL - General Track Collective Dynamics and Homeostatic Emergence in Complex Adaptive Ecosystem Dharani Punithan and RI (Bob) McKay Structural Complexity Laboratory, College of Engineering, School of Computer Science and Engineering, Seoul National University, South Korea punithan.dharani,rimsnucse @gmail.com { } Downloaded from http://direct.mit.edu/isal/proceedings-pdf/ecal2013/25/332/1901807/978-0-262-31709-2-ch049.pdf by guest on 26 September 2021 Abstract 1. Life-environment feedback via the daisyworld model We investigate the behaviour of the daisyworld model on 2. State-topology feedback via an adaptive network model an adaptive network, comparing it to previous studies on a fixed topology grid, and a fixed small-world (Newman-Watts 3. Density-growth feedback via a logistic growth model (NW)) network. The adaptive networks eventually generate topologies with small-world effect behaving similarly to the The topology of the our ecosystem evolves with a simple NW model – and radically different from the grid world. Un- der the same parameter settings, static but complex patterns local rule – a frozen habitat is reciprocally linked to an ac- emerge in the grid world. In the NW model, we see the tive habitat – and self-organises to complex topologies with emergence of completely coherent periodic dominance. In small-world effect. In this paper, we focus on the emergent the adaptive-topology world, the systems may transit through collective phenomena and properties that arise in egalitarian varied behaviours, but can self-organise to a small-world small-world ecosystems, constructed from a large number of network structure with similar cyclic behaviour to the NW model.
    [Show full text]
  • The MUCM Case Studies: Current Status and Proposals MUCM Internal Report
    The MUCM case studies: current status and proposals MUCM internal report John Paul Gosling 16th November, 2007 Abstract This internal report serves to explain the current position with regards to models and potential case studies for the MUCM project. It also pro- vides some discussion points on the direction of MUCM’s three major case studies, which are a main part of the project’s outputs. Contents 1 What is a MUCM case study? 2 2 Methodology and case studies 4 3 Models available to MUCM 7 4 Organisation of the case study workload 14 5 Case study I: biology 16 6 Case study II: environment 18 7 Case study III: engineering 20 8 Discussion and timescale 22 9 Appendix: the MUCM workpackages 23 List of Figures 1 Examplecasestudycontents. 3 2 Milestones:whenandwhat. ..................... 5 3 Arotavirusmodel........................... 17 4 Ahydrocarbonreservoirmodel . 21 5 Workpackages: numbering and methods. 23 1 1 What is a MUCM case study? The purpose of the case studies is to provide exemplars of how the MUCM meth- ods can be applied in non-trivial problems. They will illustrate combinations of techniques, and will address serious practical problems (although not necessarily offer complete solutions). Three case studies will be completed and published. The case studies will not be toy problems: in each of them, we will address questions of current and pressing concern, guided by experts on our Advisory Panel. The production of the case studies will necessarily interact with all the other aspects of the project by providing test beds for specific techniques and pulling these together into major works that are of interest to the wider scientific community.
    [Show full text]
  • Representativeness of Eddy-Covariance Flux Footprints for Areas Surrounding Ameriflux Sites
    Agricultural and Forest Meteorology 301-302 (2021) 108350 Contents lists available at ScienceDirect Agricultural and Forest Meteorology journal homepage: www.elsevier.com/locate/agrformet Representativeness of Eddy-Covariance flux footprints for areas surrounding AmeriFlux sites Housen Chu a,*, Xiangzhong Luo a,bf, Zutao Ouyang b, W. Stephen Chan a, Sigrid Dengel a, S´ebastien C. Biraud a, Margaret S. Torn a, Stefan Metzger c,d, Jitendra Kumar e, M. Altaf Arain f, Tim J. Arkebauer g, Dennis Baldocchi h, Carl Bernacchi i, Dave Billesbach g, T. Andrew Black j, Peter D. Blanken k, Gil Bohrer l, Rosvel Bracho m, Shannon Brown n, Nathaniel A. Brunsell o, Jiquan Chen p, Xingyuan Chen q, Kenneth Clark r, Ankur R. Desai d, Tomer Duman s, David Durden c, Silvano Fares t, Inke Forbrich u, John A. Gamon v,w, Christopher M. Gough x, Timothy Griffis y, Manuel Helbig z,az, David Hollinger aa, Elyn Humphreys ab, Hiroki Ikawa ac, Hiroki Iwata ad, Yang Ju l, John F. Knowles ae, Sara H. Knox af, Hideki Kobayashi ag, Thomas Kolb bg, Beverly Law aj, Xuhui Lee ak, Marcy Litvak s, Heping Liu al, J. William Munger am, Asko Noormets an, Kim Novick ao, Steven F. Oberbauer ap, Walter Oechel aq, Patty Oikawa ar, Shirley A. Papuga as, Elise Pendall at, Prajaya Prajapati an, John Prueger au, William L Quinton av, Andrew D. Richardson ah,ai, Eric S. Russell al, Russell L. Scott ae, Gregory Starr aw, Ralf Staebler ax, Paul C. Stoy d, Ellen Stuart-Ha¨entjens ay, Oliver Sonnentag az, Ryan C. Sullivan ba, Andy Suyker g, Masahito Ueyama bb, Rodrigo Vargas bc, Jeffrey D.
    [Show full text]
  • Jaarvg KS 2001/2002 Deel 1
    climate research and seismology department Biennial Scientific Report 2001–2002 2 Contents Preface Foreword Recent highlights On the role of cirrus clouds in climate 11 Pathways in the ocean 19 Monitoring of tropical processes relevant to climate change 29 Current projects Climate Variability Research 41 Oceanographic Research 48 Atmospheric Composition Research 55 Atmospheric Research 68 Climate Analysis 81 Seismology 86 Policy related and other Staff activities 93 Model support 97 Appendices Externally funded projects 101 Acronyms 105 Organisational schemes 110 List of employees 2001–2002 112 How to reach us 115 Colophon 116 3 4 Preface • In 2001 the Intergovernmental Panel on Climate Change (ipcc) published its Third Assessment Report (tar). It was concluded that “There is new and stronger evidence that most of the warming observed over the last 50 years is attributed to human activities”. Moreover “Confidence in the ability of models to project future climate has increased”. With these significant conclusions climate change continues to be an important issue on the scientific and political agenda. Per September 2001 Prof. Gerbrand Komen became Head of knmi’s Climate Research and Seismology Department, succeeding Dr. Fons Baede, who retired. By continuating its own research and by participating in various national and international networks and programmes, the Department continued to contribute to further understanding of the global climate system. It is with great pleasure that I present this fourth Biennial Scientific Report of the Department. Prof. Dr. Joost de Jong Director knmi 5 Preface 6 Foreword • knmi has a long tradition in research of the atmosphere, the ocean and the solid earth.
    [Show full text]