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100			_aPerșoiu, Ioana _951359
245			_aFlood events in Transylvania during the Medieval Warm Period and the Little Ice Age/
260			_bSage, _c2019.
300			_aVol 29, issue 1, 2019 : (85-96 p.).
520			_aWe present here the first record of past flooding activity from the Carpathian Mountains, Eastern Europe, based on documentary evidence and sedimentary records along one of the main rivers draining this region (Someșul Mic River). Three periods of increased flood activity have occurred in Transylvania during the last millennium: the first at the beginning of the 10th century (the end of the Dark Ages Cold Period and beginning of the Medieval Warm Period (MWP)); the second at the end of the 16th and beginning of 17th century, during the cold Little Ice Age (LIA) and the third at the end of the 19th century. During the early MWP, generally wet summers resulted in a high incidence of floods and/or high discharges, while the cluster of floods at the end of 16th and beginning of the 17th centuries occurred mostly at flash floods generated during heavy summer thunderstorms. Increasing winter temperatures and spring precipitations probably caused the high incidence of floods at the end of the 19th century. The predominantly wet conditions during the MWP are likely to have resulted from northward penetration of Mediterranean cyclones during a (mostly) positive phase of the North Atlantic Oscillation (NAO), while wet conditions during the LIA arose as a combination of increases in local storminess and moisture transport from the North Atlantic along more southerly positioned westerlies associated with a negative phase of the NAO.
650			_aEastern Europe, fluvial, _951360
650			_ahistorical records _951361
650			_aNorth Atlantic Oscillation, _951362
650			_apalaeohydrology, _951363
650			_asedimentology, _951328
700			_aPerșoiu, Aurel _951364
773	0		_012756 _916504 _dLondon: Sage Publication Ltd, 2019. _tHolocene/ _x09596836
856			_uhttps://doi.org/10.1177/0959683618804632
942			_2ddc _cART
999			_c12763 _d12763