FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2081569758> ?p ?o ?g. }

• W2081569758 endingPage "1129" @default.
• W2081569758 startingPage "1107" @default.
• W2081569758 abstract "The history of colluvial events over the last 8500 years is reconstructed in three Norwegian alpine slope-foot mires fed by three independent debris-flow systems. Chronologies for each site are constructed based on 155 radiocarbon-dated peat samples. At the multimillennial scale, debris-flow activity was greatest during the transition from the Holocene Thermal Maximum to the late Holocene ( c. 4300—2800 cal. BP) when debris-flow events occurred with a frequency of 1 in 33 years: two peaks in activity, characterized by 1 event in 14 years and 1 event in 25 years, were reached at the beginning and end of this interval, respectively. Least activity occurred during the Holocene Thermal Maximum from c. 8000 to 7100 cal. BP, with one event in 900 years. Eight distinct century- to millennial-scale phases of high debris-flow frequency (>3 events per 100 years) are identified at c. 8300—8000, 7100—7000, 4300—3700, 3200—2800, 2200—1900, 1500—1200, 800—700 and 300—0 cal. BP. Similarities in the records from the three sites suggest underlying climatic variations linked to the frequency of intense summer and autumn rainfall events (the primary meteorological trigger of slope failure in the source areas). Differences between the records reflect local site sensitivity to the initiation of debris-flow activity and the triggering of each subsequent debris-flow event. It is also inferred that each debris-flow system passes through multimillennial stages of at first increasing and later decreasing sensitivity as its source area expands. The climatic signals in the debris-flow record appear to differ in various respects from those derived from other precipitation-sensitive proxies from southern Norway (river floods, snow avalanches and glacier variations). Debris-flow records provide, therefore, complementary information relating to extreme climatic events and demonstrate instabilities in the Holocene landscape but provide little or no support for the concept of an increasing landscape impact of debris flows in response to global warming." @default.
• W2081569758 created "2016-06-24" @default.
• W2081569758 creator A5012060068 @default.
• W2081569758 creator A5012122355 @default.
• W2081569758 creator A5015373929 @default.
• W2081569758 creator A5020080819 @default.
• W2081569758 creator A5035267060 @default.
• W2081569758 creator A5046156219 @default.
• W2081569758 creator A5081843725 @default.
• W2081569758 date "2009-11-18" @default.
• W2081569758 modified "2023-10-18" @default.
• W2081569758 title "Radiocarbon chronology of Holocene colluvial (debris-flow) events at Sletthamn, Jotunheimen, southern Norway: a window on the changing frequency of extreme climatic events and their landscape impact" @default.
• W2081569758 cites W148865336 @default.
• W2081569758 cites W1497184485 @default.
• W2081569758 cites W1547672892 @default.
• W2081569758 cites W1888057322 @default.
• W2081569758 cites W189294987 @default.
• W2081569758 cites W1966118649 @default.
• W2081569758 cites W1968859838 @default.
• W2081569758 cites W1975644694 @default.
• W2081569758 cites W1977260115 @default.
• W2081569758 cites W1977648446 @default.
• W2081569758 cites W1979593660 @default.
• W2081569758 cites W1981515911 @default.
• W2081569758 cites W1982077758 @default.
• W2081569758 cites W1982756835 @default.
• W2081569758 cites W1983739795 @default.
• W2081569758 cites W1988331452 @default.
• W2081569758 cites W1990899433 @default.
• W2081569758 cites W1994612790 @default.
• W2081569758 cites W2000472247 @default.
• W2081569758 cites W2014890520 @default.
• W2081569758 cites W2017577481 @default.
• W2081569758 cites W2021675301 @default.
• W2081569758 cites W2022394327 @default.
• W2081569758 cites W2022800380 @default.
• W2081569758 cites W2022831043 @default.
• W2081569758 cites W2026391888 @default.
• W2081569758 cites W2030664685 @default.
• W2081569758 cites W2040423226 @default.
• W2081569758 cites W2040564200 @default.
• W2081569758 cites W2053134135 @default.
• W2081569758 cites W2054321296 @default.
• W2081569758 cites W2056137997 @default.
• W2081569758 cites W2057928160 @default.
• W2081569758 cites W2061021710 @default.
• W2081569758 cites W2064618182 @default.
• W2081569758 cites W2069329653 @default.
• W2081569758 cites W2074019336 @default.
• W2081569758 cites W2075905613 @default.
• W2081569758 cites W2080042998 @default.
• W2081569758 cites W2083662752 @default.
• W2081569758 cites W2087888479 @default.
• W2081569758 cites W2094071283 @default.
• W2081569758 cites W2094457563 @default.
• W2081569758 cites W2094718798 @default.
• W2081569758 cites W2097033979 @default.
• W2081569758 cites W2097933725 @default.
• W2081569758 cites W2098854374 @default.
• W2081569758 cites W2099411167 @default.
• W2081569758 cites W2103737089 @default.
• W2081569758 cites W2104350513 @default.
• W2081569758 cites W2115282336 @default.
• W2081569758 cites W2118909716 @default.
• W2081569758 cites W2120637384 @default.
• W2081569758 cites W2123429323 @default.
• W2081569758 cites W2136246993 @default.
• W2081569758 cites W2153106841 @default.
• W2081569758 cites W2154276443 @default.
• W2081569758 cites W2163525411 @default.
• W2081569758 cites W2280624662 @default.
• W2081569758 cites W2319341580 @default.
• W2081569758 cites W2468984683 @default.
• W2081569758 cites W2508074346 @default.
• W2081569758 cites W4210964572 @default.
• W2081569758 cites W4241335951 @default.
• W2081569758 cites W4247267616 @default.
• W2081569758 cites W4251266964 @default.
• W2081569758 cites W4252425047 @default.
• W2081569758 doi "https://doi.org/10.1177/0959683609344674" @default.
• W2081569758 hasPublicationYear "2009" @default.
• W2081569758 type Work @default.
• W2081569758 sameAs 2081569758 @default.
• W2081569758 citedByCount "33" @default.
• W2081569758 countsByYear W20815697582012 @default.
• W2081569758 countsByYear W20815697582013 @default.
• W2081569758 countsByYear W20815697582014 @default.
• W2081569758 countsByYear W20815697582015 @default.
• W2081569758 countsByYear W20815697582016 @default.
• W2081569758 countsByYear W20815697582017 @default.
• W2081569758 countsByYear W20815697582018 @default.
• W2081569758 countsByYear W20815697582019 @default.
• W2081569758 countsByYear W20815697582020 @default.
• W2081569758 countsByYear W20815697582022 @default.
• W2081569758 crossrefType "journal-article" @default.
• W2081569758 hasAuthorship W2081569758A5012060068 @default.
• W2081569758 hasAuthorship W2081569758A5012122355 @default.
• W2081569758 hasAuthorship W2081569758A5015373929 @default.

• next