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"Arensburg" is a misspelling and links to the Estonian city of Kuressaare (formerly Arensburg) which has nothing to do with the intended Paleolithic culture. The correct spelling is " Ahrensburg", a Terminal Paleolithic culture that is named after a locality in northern Germany.-- Death Bredon 16:09, 11 May 2007 (UTC)
Allerød doesn't belong to the Furesø_Municipality — Preceding unsigned comment added by 89.23.239.99 ( talk) 13:54, 4 October 2017 (UTC)
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1) [1] https://pubs.geoscienceworld.org/gsa/geology/article-abstract/33/2/89/129325/Catastrophic-meltwater-discharge-down-the-Hudson
From that link: "Glacial freshwater discharge to the Atlantic Ocean during deglaciation may have inhibited oceanic thermohaline circulation, and is often postulated to have driven climatic fluctuations. Yet attributing meltwater-discharge events to particular climate oscillations is problematic, because the location, timing, and amount of meltwater discharge are often poorly constrained. We present evidence from the Hudson Valley and the northeastern U.S. continental margin that establishes the timing of the catastrophic draining of Glacial Lake Iroquois, which breached the moraine dam at the Narrows in New York City, eroded glacial lake sediments in the Hudson Valley, and deposited large sediment lobes on the New York and New Jersey continental shelf ca. 13,350 yr B.P. Excess 14C in Cariaco Basin sediments indicates a slowing in thermohaline circulation and heat transport to the North Atlantic at that time, and both marine and terrestrial paleoclimate proxy records around the North Atlantic show a short-lived (<400 yr) cold event (Intra-Allerød cold period) that began ca. 13,350 yr B.P. The meltwater discharge out the Hudson Valley may have played an important role in triggering the Intra-Allerød cold period by diminishing thermohaline circulation."
2) [2] https://ui.adsabs.harvard.edu/abs/2020AGUFMPP0410010P/abstract
From that link: "It has long been hypothesized that periodic meltwater input from a retreating Laurentide Ice Sheet (LIS) inhibited North Atlantic deep water (NADW) formation, weakened the strength of the Atlantic Meridional Overturning Circulation (AMOC), and triggered several cold periods in the North Atlantic region during the last deglaciation (21-8ka yrs BP). Since the establishment of this hypothesis more than thirty years ago, geomorphic and chronologic evidence of meltwater flows from the LIS have been shown to roughly coincide with centennial-to-millennial scale cool periods (e.g., Younger Dryas, the 8.2 ka event). The complexity of LIS meltwater routing during deglaciation, a lack of tight spatial and temporal constraint on meltwater events and volumes, and insights from models have however made it difficult to point to a specific meltwater event as the trigger for a particular cold period. Here, we use a numerical model to investigate the possibility of meltwater discharge from the Hudson River, New York City, USA ~13,350 yrs BP as a potential trigger of the Inter-Allerød Cold Period (IACP). Using flood volumes estimated from paleoshorelines, we assess the sensitivity of AMOC to both short duration (1 month), and long duration (1 year) flood events. We also assess the impact of successive flood events on AMOC to determine if sequential floods impact AMOC differently than a single flood event. We find that in all of our experiments (regardless of flood magnitude, duration, or reoccurrence interval) there is no significant weakening of the AMOC. This limited impact suggests that although the Hudson Valley floods likely occur close to the beginning of the IACP, it is unlikely the trigger. Further observations to constrain the timing of the Hudson Valley Floods and additional modeling experiments exploring different and/or multiple meltwater inputs are needed to determine if meltwater inputs from the LIS could have been a trigger and/or contributor of the IACP. Our results have significant implications for determining whether other deglacial flood events triggered periods of climatic cooling: for example, the millennial-length Younger Dryas cooling is thought to have been triggered by a flood only 3-times larger than the one from the Hudson River, which again questions the role meltwater played in triggering climate cooling."
Obviously, the two articles contradict each other. The first is from 2005; the second is from 2020. Frunobulax ( talk) 01:45, 9 August 2023 (UTC)
![]() | It was proposed in this section that multiple pages be
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result: Move logs:
source title ·
target title
This is template {{
subst:Requested move/end}} |
– Allerød oscillation is a rarely used name for a climatic period. Allerød is far more common and is not used on its own in any other sense, but it has been used for a disambiguation page. I have moved Allerod to Allerød (disambiguation) and would now like to complete the move. Dudley Miles ( talk) 11:02, 9 August 2023 (UTC) This is a contested technical request ( permalink). Dudley Miles ( talk) 14:08, 9 August 2023 (UTC) — Relisting. CLYDE TALK TO ME/ STUFF DONE 19:32, 16 August 2023 (UTC)
![]() | This redirect does not require a rating on Wikipedia's
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"Arensburg" is a misspelling and links to the Estonian city of Kuressaare (formerly Arensburg) which has nothing to do with the intended Paleolithic culture. The correct spelling is " Ahrensburg", a Terminal Paleolithic culture that is named after a locality in northern Germany.-- Death Bredon 16:09, 11 May 2007 (UTC)
Allerød doesn't belong to the Furesø_Municipality — Preceding unsigned comment added by 89.23.239.99 ( talk) 13:54, 4 October 2017 (UTC)
Hello fellow Wikipedians,
I have just modified one external link on Allerød oscillation. Please take a moment to review my edit. If you have any questions, or need the bot to ignore the links, or the page altogether, please visit this simple FaQ for additional information. I made the following changes:
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This message was posted before February 2018.
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regular verification using the archive tool instructions below. Editors
have permission to delete these "External links modified" talk page sections if they want to de-clutter talk pages, but see the
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(last update: 5 June 2024).
Cheers.— InternetArchiveBot ( Report bug) 05:29, 23 January 2018 (UTC)
1) [1] https://pubs.geoscienceworld.org/gsa/geology/article-abstract/33/2/89/129325/Catastrophic-meltwater-discharge-down-the-Hudson
From that link: "Glacial freshwater discharge to the Atlantic Ocean during deglaciation may have inhibited oceanic thermohaline circulation, and is often postulated to have driven climatic fluctuations. Yet attributing meltwater-discharge events to particular climate oscillations is problematic, because the location, timing, and amount of meltwater discharge are often poorly constrained. We present evidence from the Hudson Valley and the northeastern U.S. continental margin that establishes the timing of the catastrophic draining of Glacial Lake Iroquois, which breached the moraine dam at the Narrows in New York City, eroded glacial lake sediments in the Hudson Valley, and deposited large sediment lobes on the New York and New Jersey continental shelf ca. 13,350 yr B.P. Excess 14C in Cariaco Basin sediments indicates a slowing in thermohaline circulation and heat transport to the North Atlantic at that time, and both marine and terrestrial paleoclimate proxy records around the North Atlantic show a short-lived (<400 yr) cold event (Intra-Allerød cold period) that began ca. 13,350 yr B.P. The meltwater discharge out the Hudson Valley may have played an important role in triggering the Intra-Allerød cold period by diminishing thermohaline circulation."
2) [2] https://ui.adsabs.harvard.edu/abs/2020AGUFMPP0410010P/abstract
From that link: "It has long been hypothesized that periodic meltwater input from a retreating Laurentide Ice Sheet (LIS) inhibited North Atlantic deep water (NADW) formation, weakened the strength of the Atlantic Meridional Overturning Circulation (AMOC), and triggered several cold periods in the North Atlantic region during the last deglaciation (21-8ka yrs BP). Since the establishment of this hypothesis more than thirty years ago, geomorphic and chronologic evidence of meltwater flows from the LIS have been shown to roughly coincide with centennial-to-millennial scale cool periods (e.g., Younger Dryas, the 8.2 ka event). The complexity of LIS meltwater routing during deglaciation, a lack of tight spatial and temporal constraint on meltwater events and volumes, and insights from models have however made it difficult to point to a specific meltwater event as the trigger for a particular cold period. Here, we use a numerical model to investigate the possibility of meltwater discharge from the Hudson River, New York City, USA ~13,350 yrs BP as a potential trigger of the Inter-Allerød Cold Period (IACP). Using flood volumes estimated from paleoshorelines, we assess the sensitivity of AMOC to both short duration (1 month), and long duration (1 year) flood events. We also assess the impact of successive flood events on AMOC to determine if sequential floods impact AMOC differently than a single flood event. We find that in all of our experiments (regardless of flood magnitude, duration, or reoccurrence interval) there is no significant weakening of the AMOC. This limited impact suggests that although the Hudson Valley floods likely occur close to the beginning of the IACP, it is unlikely the trigger. Further observations to constrain the timing of the Hudson Valley Floods and additional modeling experiments exploring different and/or multiple meltwater inputs are needed to determine if meltwater inputs from the LIS could have been a trigger and/or contributor of the IACP. Our results have significant implications for determining whether other deglacial flood events triggered periods of climatic cooling: for example, the millennial-length Younger Dryas cooling is thought to have been triggered by a flood only 3-times larger than the one from the Hudson River, which again questions the role meltwater played in triggering climate cooling."
Obviously, the two articles contradict each other. The first is from 2005; the second is from 2020. Frunobulax ( talk) 01:45, 9 August 2023 (UTC)
![]() | It was proposed in this section that multiple pages be
renamed and moved.
result: Move logs:
source title ·
target title
This is template {{
subst:Requested move/end}} |
– Allerød oscillation is a rarely used name for a climatic period. Allerød is far more common and is not used on its own in any other sense, but it has been used for a disambiguation page. I have moved Allerod to Allerød (disambiguation) and would now like to complete the move. Dudley Miles ( talk) 11:02, 9 August 2023 (UTC) This is a contested technical request ( permalink). Dudley Miles ( talk) 14:08, 9 August 2023 (UTC) — Relisting. CLYDE TALK TO ME/ STUFF DONE 19:32, 16 August 2023 (UTC)