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GEOMORPHOLOGICAL CHANGES WITHIN A HILLSLOPE CAUSED BY A WINDTHROW EVENT IN THE TATRA MOUNTAINS, SOUTHERN POLAND Geogr. Ann. Ser. A Phys. Geogr. (IF 1.652) Pub Date : 2016-12-05 DARIUSZ STRZYŻOWSKI, JOANNA FIDELUS, MIROSŁAW ŻELAZNY
Tree uprooting plays an important role in hillslope evolution. The geomorphological impact of tree uprooting after a foehn wind occurrence, in December 2013 in the Tatra Mountains, was investigated. Geomorphological mapping was conducted in three watersheds. Additionally, in one of the watersheds, 459 windthrow pits were measured, in an area of 6.4 ha. The mean volume of a pit was 2.41 m3, and the
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GPS PERFORMANCE IN YUKON'S ARCTIC COAST Geogr. Ann. Ser. A Phys. Geogr. (IF 1.652) Pub Date : 2016-12-05 DAVID SWANLUND, RAMONA MARAJ, NADINE SCHUURMAN, ROXANNE HOPE, KATE DONKERS, MATT AQUIN, GWEN RICKERBY
This study analyses GPS performance in Yukon's Arctic coast to inform future research that uses this technology in the region. To test this, Telonics GPS collars were placed on stakes during the summers of 2009 and 2010 throughout the region for varying lengths of time. The fix records produced by these collars were then collected and cleaned, leaving 30 samples. Using these records combined with a
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SPATIO‐TEMPORAL SPECIFICS OF HYDRO‐GEOMORPHIC PROCESSES IN HEADWATER PARTS OF MID‐MOUNTAINS RECONSTRUCTED BASED ON TREE‐RING DATA: A CASE STUDY FROM THE HRUBÝ JESENÍK MOUNTAINS (CZECH REPUBLIC) Geogr. Ann. Ser. A Phys. Geogr. (IF 1.652) Pub Date : 2016-12-05 RADEK TICHAVSKÝ, KAREL ŠILHÁN
Debris flows and debris floods cause frequent geomorphic hazards, even in the mid‐mountains of Central Europe. In the Hrubý Jeseník Mountains (Eastern Sudetes, Czech Republic), strong anthropogenic interventions have created specific conditions for erosion, transport and accumulation of material released by debris flow/flood events. We present a detailed spatio‐temporal reconstruction of the hydro‐geomorphic
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TRACE ELEMENT DISTRIBUTION AND IMPLICATIONS IN SEDIMENTS ACROSS THE ALLERØD–YOUNGER DRYAS BOUNDARY IN THE NETHERLANDS AND BELGIUM Geogr. Ann. Ser. A Phys. Geogr. (IF 1.652) Pub Date : 2016-09-06 ALEXANDRE V. ANDRONIKOV, ANNELIES VAN HOESEL, IRINA E. ANDRONIKOVA, WIM Z. HOEK
In the Northern Hemisphere, the Younger Dryas cooling occurred between 12.8 and 11.7 ka bp. This cooling is thought to have been the result of an abrupt change in atmospheric and oceanic circulations. One of the hypotheses explaining such a change suggests that just before the onset of the Younger Dryas cooling, multiple airbursts/impacts occurred over the Northern Hemisphere. We studied the late Pleistocene
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IS THE EXTREME SNOW DEPTH RECORD FOR NORDLAND, NORWAY RELIABLE? Geogr. Ann. Ser. A Phys. Geogr. (IF 1.652) Pub Date : 2016-08-04 WILFRED H. THEAKSTONE
A snow depth of 370 cm at Dunderlandsdalen in winter 1919–20 is the largest recorded at stations in Nordland, Norway. During the period 1895–1924, the average maximum annual value there was 150.4 cm; at other stations it ranged from 38.5 to 190.1 cm. The ratio of maxima at other stations to that at Dunderlandsdalen was particularly low in 1919–20. In Nordland generally, that winter's recorded precipitation
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THE ROLE OF ATMOSPHERIC CIRCULATION PATTERNS IN AGROCLIMATE VARIABILITY IN FINLAND, 1961–2011 Geogr. Ann. Ser. A Phys. Geogr. (IF 1.652) Pub Date : 2016-08-02 MASOUD IRANNEZHAD, DELIANG CHEN, BJØRN KLØVE
This study evaluates interannual variations and trends in growing season daily temperature sum and daily precipitation sum in Finland during 1961–2011, and their connections to well known atmospheric circulation patterns. Changes in summer (June–August) climate partially explain changes in growing season daily temperature sum and daily precipitation sum over Finland, which naturally decreased from
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A STATISTICAL FRAMEWORK FOR TREE‐RING RECONSTRUCTION OF HIGH‐MAGNITUDE MASS MOVEMENTS: CASE STUDY OF SNOW AVALANCHES IN EASTERN CANADA Geogr. Ann. Ser. A Phys. Geogr. (IF 1.652) Pub Date : 2016-08-02 DANIEL GERMAIN
This paper investigates the application of the peaks‐over‐threshold method in combination with fitting of the generalized Pareto distribution for estimating the frequency of high‐magnitude geomorphic events, on the basis of tree‐ring data. In particular, attention is focused on extreme value distribution of tree‐ring responses and in the minimum threshold or index number required to assure the past