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note
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Acknowledgements. The programs on which this paper is based were financed by the Swedish Natural Science Research Council (NFR) and The Environment and Space Research Institute (MRI). Thanks also to Rickard Pettersson for his support in preparing data from Mårmaglaciaren, and a special thanks to Anna Schytt for all her help in interpreting and compiling messages from the Antarctic continent where I was on field-work during the final phase of writing the paper
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