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136 CHAPTER 3. TERRESTRIAL SYSTEMS Roth, K., Boike, J., & Vogel, H.-J. 2005. Quantifying Permafrost Patterns using Minkowski Densities. Permafrost and Periglacial Processes, 16, 277–290, doi: 10.1002/ppp.531. Stöhr, M., & Roth, K. 2005. Gradient-based estimation of local parameters for flow and transport in heterogeneous porous media. Water Resour. Res., 41, 1–14, W08401, doi:10.1029/2004WR003768. Topp, G. C., Davis, J. L., & Annan, A. P. 1980. Electromagnetic determination of soil water content: Measurement in coaxial transmission lines. Water Resour. Res., 16, 574–582. Ulbrich, C. 2005. Monitoring Field Tracer Experiment with Ground Penetrating Radar and Time Domain Reflectometry. Diplomarbeit, University of Heidelberg. Vogel, H.-J. 2005a. From Pore- to Continuum-Scale Understanding of Flow and Transport Processes in Porous Media. Keynote paper, SSSA-Annual Meeting, November 7-11, 2005, Salt Lake City, USA. Vogel, H.-J. 2005b. Hierarchies of flow and transport in soil. Keynote paper, GFHN, 29emes journees, November 24-25, 2004, Grenoble, France. Vogel, H.-J. 2005c. Modeling the heterogeneous structure of soil to predict flow and transport. SIAM Conference on Mathematical and Computational Issues in the Geosciences, June 7-10, 2005, Avignon, France. Vogel, H.-J., Tölke, J., Schulz, V. P., Krafczyk, M., & Roth, K. 2005a. Comparison of a Lattice- Boltzmann Model, a Full-Morphology Model, and a Pore Network Model for Determining Capillary Pressure-Saturation Relationships. Vadose Zone J., 4, 380–388, doi: 10.2136/vzj2004.0114. Vogel, H.-J., Cousin, I., Ippisch, O., & Bastian, P. 2005b. The dominant role of structure for solute transport in soil: Experimental evidence and modelling of structure and transport in a field experiment. Hydrology and Earth System Sciences Discussion, 2, 2153–2181, SRef–ID: 1812– 2116/hessd/2005–2–1. Vogel, H.-J., Samouelian, A., & Ippisch, O. 2005c. Modeling structure to predict flow and transport. Gesellschaft <strong>für</strong> Angewandte Mathematik und Mechanik, 76th Annual Scientific Conference, March 28 - April 1, 2005, Luxembourg. Vogel, H.-J., Hoffmann, H., & Roth, K. 2005d. Studies of crack dynamics in clay soil. I. Experimental methods, results, and morphological quantification. Geoderma, 125, 203–211. Vogel, H.-J., Hoffmann, H., Leopold, A., & Roth, K. 2005e. Studies of crack dynamics in clay soil. II. A physically based model for crack formation. Geoderma, 125, 213–223. Wollschläger, U., & Roth, K. 2004. Estimating the three-dimensional hydraulic structure of soils from ground-penetrating radar measurements. Pages 501–504 of: Proceedings of the 10th International Conference on Ground Penetrating Radar, Delft. Wollschläger, U., & Roth, K. 2005. Estimation of temporal changes of volumetric soil water content from ground-penetrating radar reflections. Subsurf. Sens. Technol. Appl., 6(2), doi: 10.1007/s11220– 005–0007–y. Yu, Q., Shi, C., Niu, F., He, N., & Roth, K. 2005. Analysis of temperature controlled ventilated embankment. Cold Reg. Sci. Technol., 42, 17–24, doi:10.1016/j.coldregions.2004.11.004.
3.2. ICE AND CLIMATE 137 3.2 Ice and Climate Names of group members Isabel Bengel, diploma student Felix Jahn, diploma student Barbara May, diploma student Christine Offermann, diploma student Dipl.Phys. Markus Pettinger, PhD student Dipl.Phys. Martin Schock, PhD student Dr. Dietmar Wagenbach, head of group Overarching topic, main methods and specific objectives Among all paleo-archives, only non-temperated glaciers basically allow the reconstruction of climate as well as of environmental records. Appropriate ice core studies may thus allow to tackle the crucial problem about the mutual relationships between changes of climate and bio-geochemical cycles through a retrospective approach. Figure 3.14: Drilling down to bedrock at Colle Gnifetti (Monte Rosa 4500m a.s.l.) September 2005. View on the exposed situation of the drill camp near the ice-cliff (dome drilling tent at upper right rim). Picture: Olaf Eisen In this context, the ’Ice and Climate’ group concentrates on ice core investigations by deploying the following species, backed up by standard physical ice properties: • water-isotopomeres δ 18 O- δD (thermometry) • various particulate key species as mineral dust, major ions, organic carbon (bio-geochemical cycles), • natural radionuclides as terrestrial 210 Pb, cosmogenic 10 Be, 3 H, 36 Cl (solar variability)and on 3 He, 4 He isotopes (basal layer dynamics). Apart from joint activities within polar ice core studies, emphasis is thereby on the independent exploration of non-temperated alpine glaciers. Such small scale drill sites are unique in supplementing high latitude ice core findings, though reliable atmospheric signals would be much more difficult to elucidate here (Preunkert et al., 2000). In addition to ice core analyses, deserving application of novel techniques and species (Ruth et al., 2003), also process-oriented field studies are regularly performed. These specific activities are aimed at understanding the transfer of the atmospheric signals into the glacier archive as well as at constraining their basic glaciological embedding conditions (as e.g.
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Contents 1 Introduction/Overview of
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CONTENTS 7 3.2.1 Glaciological pilo
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Introduction In Heidelberg, environ
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Overview Summary Atmospheric resear
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2.3. RADIATIVE TRANSFER 45 2.3 Radi
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2.3. RADIATIVE TRANSFER 47 Funding
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7.3. PHD THESES 217 PhD Theses Baye
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7.5. INVITED TALKS 221 Invited Talk
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7.5. INVITED TALKS 223 Pundt, I. 20
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Institut für Umweltphysik Im Neuen
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