997 resultados para Franz-josef glacier
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Bernhard Mandl
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von Adolf Blumenthal
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von Arthur S. Weissmann
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von Arthur S. Weissmann
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Glacier fluctuations are a key indicator of changing climate. Their reconstruction beyond historical times unravels glacier variability and its forcing factors on long time scales, which can considerably improve our understanding of the climate–glacier relationship. Here, we present a 2250-year-long reconstruction of particle-mass accumulation rates recorded in the lacustrine sediments of Lake Trüebsee (Central Swiss Alps) that are directly related to glacier extent, thus reflecting a continuous record of fluctuations of the upstream-located Titlis Glacier. Mass accumulation rate values show strong centennial to multi-centennial fluctuations and reveal 12 well-pronounced periods of enhanced values corresponding to times of maximum extent of the neighboring Lower Grindelwald Glacier. This result supports previous studies of proglacial lake sediments that documented high mass accumulation rate values during glacier advances. The strong variability in the Lake Trüebsee mass accumulation rate record thus represents a highly sensitive paleoclimatic archive, which mirrors rapid and pronounced feedbacks of Titlis Glacier to climatic changes over the past 2250years. The comparison of our data with independent paleo-temperature reconstructions from tree rings suggests that variations in mean summer temperature were the primary driving factor of fluctuations of Titlis Glacier. Also, advances of Titlis Glacier occurred during the grand solar minima (Dalton, Maunder, Spörer, Wolf) of the last millennium. This relation of glacier extent with summer temperature reveals strong evidence that the mass balance of this Alpine glacier is primarily controlled by the intensity of glacier melting during summer.
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Literaturverz. S. 9-10
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Gesellschaft der Freunde
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bearb. von Manfred Zimmermann
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BACKGROUND The Sorin Freedom SOLO (FS) bovine pericardial stentless valve prosthesis is designed for supraannular, subcoronary implantation. We report our experience and results with 277 consecutively implanted FS bioprostheses. METHODS 277 patients (mean age, 74.2 ± 7.3 years; 139 (50.2%) female) underwent aortic valve replacement (AVR) with the FS stentless bioprosthesis. The hemodynamic performance was investigated with transthoracic echocardiography at discharge, 6 months later, and yearly thereafter. Follow-up was 100% complete, with an average observation time of 2.6 ± 1.7 years and a total of 697.3 patient-years. RESULTS The overall 30-day mortality was 4.3%. The mortalities for isolated AVR and combined procedures were 1.9% and 7.3%, respectively. No causes of death were valve-related. Preoperative peak (74.2 ± 23.0 mm Hg) and mean (48.6 ± 16.3 mm Hg) gradients decreased to 15.6 ± 5.4 mm Hg and 8.8 ± 3.0 mm Hg postoperatively and remained unchanged for as long as 5 years. The postoperative mean effective orifice area (EOA) for valve sizes 19, 21, 23, 25, and 27 were 1.49 ± 0.32 cm(2), 1.67 ± 0.40 cm(2), 1.92 ± 0.38 cm(2), 2.01 ± 0.42 cm(2), and 2.13 ± 0.36 cm(2), respectively. Severe prosthesis-patient mismach (PPM) was completely absent, and moderate PPM occurred in 17 patients (6.1%). In isolated AVR, 0.8% of patients with preoperative sinus rhythm required a permanent pacemaker before hospital discharge. There was 100% freedom from structural valve deterioration, 99.6 % freedom from endocarditis and reoperation, and 97.3% freedom from thromboembolism at 5 years. CONCLUSIONS The FS stentless aortic valve is safe to implant, and it shows excellent hemodynamic performance and early and midterm results. Owing to the favorable EOA, the valve appears particularly attractive for patients at risk for PPM.