The Experts below are selected from a list of 306 Experts worldwide ranked by ideXlab platform
I. H. Schmidt - One of the best experts on this subject based on the ideXlab platform.
-
Permafrost aggradation and peat accumulation since 1200 years B.P. in peat Plateaus at Tuchitua, Yukon Territory (Canada)
Journal of Paleolimnology, 1994Co-Authors: S. A. Harris, I. H. SchmidtAbstract:Floating and grounded peat Plateaus were studied in fens in the Yukon Territory (Canada). The peat deposit may be over 4 m thick and consists of a lower bed of aquatic peat overlain by humic fen peat, mesic fen peat and woody peat. Permafrost in the grounded peat Plateaus is older than the 1200 year old White River Ash, whereas permafrost in the floating peat plateau is younger. Peat accumulation rates since 1200 years B.P. were greater in the fens (85–100 cm) than on the surface of the peat Plateaus (25–55 cm). Where the peat plateau is free-floating, it will persist until the climate changes, causing the icy core to thaw. Where the peat plateau is frozen to the mineral substrate, it slowly drowns since the fen peat accumulates faster than the woody peat. This drowning results in degradation of the landform independently of the climate. Only degradation of floating peat Plateaus can be used to identify climatic changes.
-
Permafrost aggradation and peat accumulation since 1200 years B.P. in peat Plateaus at Tuchitua, Yukon Territory (Canada)
Journal of Paleolimnology, 1994Co-Authors: S. A. Harris, I. H. SchmidtAbstract:Floating and grounded peat Plateaus were studied in fens in the Yukon Territory (Canada). The peat deposit may be over 4 m thick and consists of a lower bed of aquatic peat overlain by humic fen peat, mesic fen peat and woody peat. Permafrost in the grounded peat Plateaus is older than the 1200 year old White River Ash, whereas permafrost in the floating peat plateau is younger.
Andre F Lotter - One of the best experts on this subject based on the ideXlab platform.
-
late glacial radiocarbon and palynostratigraphy on the swiss plateau
Boreas, 2008Co-Authors: Brigitta Ammann, Andre F LotterAbstract:A detailed late-glacial radiocarbon stratigraphy for the Swiss Plateau has been established on the basis of over 90 accelerator 14C dates on terrestrial plant macrofossils. Two plateaux of constant.,14C age were observed, occurring at 12,700 B.P. and at 10,000 B.P. The consequences of these plateaux for palaeo-ecological investigations are threefold: (1) a more refined 14C dating within the plateaux is not possible, (2) in teleconnections between different sites (if based on 14C dating and concerning the periods around 12,700 B.P. and 10,000 B.P.) events are considered synchronous which are only synchronous within a plateau of constant age, and (3) exact time-depth relationship and therefore influx calculations are made impossible during these plateau periods. A comparison of the radiocarbon ages derived from terrestrial, telmatic and limnic material at different sites on the Swiss Plateau yields a proposal for modifying the zonation system of Welten for the Late-Glacial. By retaining the limits of chronozones (at 13, 12, 11 and 10ka B.P.) and by refining the palynostratigraphic criteria for the limits of biozones, a separation between chrono- and biozonation at the beginning of the Belling and at the beginning of the Younger Dryas becomes obvious.
-
Late‐Glacial radiocarbon‐ and palynostratigraphy on the Swiss Plateau
Boreas, 2008Co-Authors: Brigitta Ammann, Andre F LotterAbstract:A detailed late-glacial radiocarbon stratigraphy for the Swiss Plateau has been established on the basis of over 90 accelerator 14C dates on terrestrial plant macrofossils. Two plateaux of constant.,14C age were observed, occurring at 12,700 B.P. and at 10,000 B.P. The consequences of these plateaux for palaeo-ecological investigations are threefold: (1) a more refined 14C dating within the plateaux is not possible, (2) in teleconnections between different sites (if based on 14C dating and concerning the periods around 12,700 B.P. and 10,000 B.P.) events are considered synchronous which are only synchronous within a plateau of constant age, and (3) exact time-depth relationship and therefore influx calculations are made impossible during these plateau periods. A comparison of the radiocarbon ages derived from terrestrial, telmatic and limnic material at different sites on the Swiss Plateau yields a proposal for modifying the zonation system of Welten for the Late-Glacial. By retaining the limits of chronozones (at 13, 12, 11 and 10ka B.P.) and by refining the palynostratigraphic criteria for the limits of biozones, a separation between chrono- and biozonation at the beginning of the Belling and at the beginning of the Younger Dryas becomes obvious.
S. A. Harris - One of the best experts on this subject based on the ideXlab platform.
-
Permafrost aggradation and peat accumulation since 1200 years B.P. in peat Plateaus at Tuchitua, Yukon Territory (Canada)
Journal of Paleolimnology, 1994Co-Authors: S. A. Harris, I. H. SchmidtAbstract:Floating and grounded peat Plateaus were studied in fens in the Yukon Territory (Canada). The peat deposit may be over 4 m thick and consists of a lower bed of aquatic peat overlain by humic fen peat, mesic fen peat and woody peat. Permafrost in the grounded peat Plateaus is older than the 1200 year old White River Ash, whereas permafrost in the floating peat plateau is younger. Peat accumulation rates since 1200 years B.P. were greater in the fens (85–100 cm) than on the surface of the peat Plateaus (25–55 cm). Where the peat plateau is free-floating, it will persist until the climate changes, causing the icy core to thaw. Where the peat plateau is frozen to the mineral substrate, it slowly drowns since the fen peat accumulates faster than the woody peat. This drowning results in degradation of the landform independently of the climate. Only degradation of floating peat Plateaus can be used to identify climatic changes.
-
Permafrost aggradation and peat accumulation since 1200 years B.P. in peat Plateaus at Tuchitua, Yukon Territory (Canada)
Journal of Paleolimnology, 1994Co-Authors: S. A. Harris, I. H. SchmidtAbstract:Floating and grounded peat Plateaus were studied in fens in the Yukon Territory (Canada). The peat deposit may be over 4 m thick and consists of a lower bed of aquatic peat overlain by humic fen peat, mesic fen peat and woody peat. Permafrost in the grounded peat Plateaus is older than the 1200 year old White River Ash, whereas permafrost in the floating peat plateau is younger.
A Panaitescu - One of the best experts on this subject based on the ideXlab platform.
-
x ray flares Plateaus and chromatic breaks of grb afterglows from up scattered forward shock emission
Monthly Notices of the Royal Astronomical Society, 2007Co-Authors: A PanaitescuAbstract:Scattering of the forward-shock synchrotron emission by a relativistic outflow located behind the leading blast wave may produce an X-ray emission brighter than that coming directly from the forward shock and may explain four features displayed by Swift X-ray afterglows: flares, Plateaus (slow decays), chromatic light-curve breaks and fast post-plateau decays. For a cold scattering outflow, the reflected flux overshines the primary one if the scattering outflow is nearly baryon-free and highly relativistic. These two requirements can be relaxed if the scattering outflow is energized by weak internal shocks, so that the incident forward-shock photons are also inverse-Compton scattered, in addition to bulk scattering. Sweeping-up of the photons left behind by the forward shock naturally yields short X-ray flares. Owing to the boost in photon energy produced by bulk scattering, the reflected emission is more likely to overshine that coming directly from the forward shock at higher photon energies, yielding light-curve Plateaus and breaks that appear only in the X-ray. The brightness, shape and decay of the X-ray light-curve plateau depend on the radial distribution of the scatterer's Lorentz factor and mass flux. Chromatic X-ray light-curve breaks and sharp post-plateau decays cannot be accommodated by the direct forward-shock emission and argue in favour of the scattering-outflow model proposed here. On the other hand, the X-ray afterglows without Plateaus, those with achromatic breaks and those with very long lived power-law decays are more naturally accommodated by the standard forward-shock model. Thus, the diversity of X-ray light curves arises from the interplay of the scattered and direct forward-shock emissions.
-
x ray flares Plateaus and chromatic breaks of grb afterglows from up scattered forward shock emission
arXiv: Astrophysics, 2007Co-Authors: A PanaitescuAbstract:Scattering of the forward-shock synchrotron emission by a relativistic outflow located behind the leading blast-wave may produce an X-ray emission brighter than that coming directly from the forward-shock and may explain four features displayed by Swift X-ray afterglows: flares, Plateaus (slow decays), chromatic light-curve breaks, and fast post-plateau decays. For a cold scattering outflow, the reflected flux overshines the primary one if the scattering outflow is nearly baryon-free and highly relativistic. These two requirements can be relaxed if the scattering outflow is energized by weak internal shocks, so that the incident forward-shock photons are also inverse-Compton scattered, in addition to bulk-scattering. Sweeping-up of the photons left behind by the forward shock naturally yields short X-ray flares. Owing to the boost in photon energy produced by bulk-scattering scattering, the reflected emission is more likely to overshine that coming directly from the forward shock at higher photon energies, yielding light-curve Plateaus and breaks that appear only in the X-ray. The brightness, shape, and decay of the X-ray light-curve plateau depend on the radial distribution of the scatterer's Lorentz factor and mass-flux. Chromatic X-ray light-curve breaks and sharp post-plateau decays cannot be accommodated by the direct forward-shock emission and argue in favour of the scattering-outflow model proposed here. On the other hand, the X-ray afterglows without Plateaus, those with achromatic breaks, and those with very long-lived power-law decays are more naturally accommodated by the standard forward-shock model. Thus the diversity of X-ray light-curves arises from the interplay of the scattered and direct forward-shock emissions.
Brigitta Ammann - One of the best experts on this subject based on the ideXlab platform.
-
late glacial radiocarbon and palynostratigraphy on the swiss plateau
Boreas, 2008Co-Authors: Brigitta Ammann, Andre F LotterAbstract:A detailed late-glacial radiocarbon stratigraphy for the Swiss Plateau has been established on the basis of over 90 accelerator 14C dates on terrestrial plant macrofossils. Two plateaux of constant.,14C age were observed, occurring at 12,700 B.P. and at 10,000 B.P. The consequences of these plateaux for palaeo-ecological investigations are threefold: (1) a more refined 14C dating within the plateaux is not possible, (2) in teleconnections between different sites (if based on 14C dating and concerning the periods around 12,700 B.P. and 10,000 B.P.) events are considered synchronous which are only synchronous within a plateau of constant age, and (3) exact time-depth relationship and therefore influx calculations are made impossible during these plateau periods. A comparison of the radiocarbon ages derived from terrestrial, telmatic and limnic material at different sites on the Swiss Plateau yields a proposal for modifying the zonation system of Welten for the Late-Glacial. By retaining the limits of chronozones (at 13, 12, 11 and 10ka B.P.) and by refining the palynostratigraphic criteria for the limits of biozones, a separation between chrono- and biozonation at the beginning of the Belling and at the beginning of the Younger Dryas becomes obvious.
-
Late‐Glacial radiocarbon‐ and palynostratigraphy on the Swiss Plateau
Boreas, 2008Co-Authors: Brigitta Ammann, Andre F LotterAbstract:A detailed late-glacial radiocarbon stratigraphy for the Swiss Plateau has been established on the basis of over 90 accelerator 14C dates on terrestrial plant macrofossils. Two plateaux of constant.,14C age were observed, occurring at 12,700 B.P. and at 10,000 B.P. The consequences of these plateaux for palaeo-ecological investigations are threefold: (1) a more refined 14C dating within the plateaux is not possible, (2) in teleconnections between different sites (if based on 14C dating and concerning the periods around 12,700 B.P. and 10,000 B.P.) events are considered synchronous which are only synchronous within a plateau of constant age, and (3) exact time-depth relationship and therefore influx calculations are made impossible during these plateau periods. A comparison of the radiocarbon ages derived from terrestrial, telmatic and limnic material at different sites on the Swiss Plateau yields a proposal for modifying the zonation system of Welten for the Late-Glacial. By retaining the limits of chronozones (at 13, 12, 11 and 10ka B.P.) and by refining the palynostratigraphic criteria for the limits of biozones, a separation between chrono- and biozonation at the beginning of the Belling and at the beginning of the Younger Dryas becomes obvious.
