Data for: The evolution of the Patagonian Ice Sheet from 35 ka to the Present Day (PATICE), v1. Davies, Bethan (Author); Darvill, Christopher (Author); Lovell, Harold (Author); Bendle, Jacob (Author); Dowdeswell, Julian A. (Author); Fabel, Derek (Author); Garcia, Juan-Luis (Author); Geiger, Alessa (Author); Glasser, Neil F. (Author); Gheorghiu, Delia (Author); Harrison, Stephan (Author); Hein, Andrew S. (Author); Kaplan, Michael (Author); Martin, Julian (Author); Mendelova, Monika (Author); Palmer, Adrian (Author); Pelto, Mauri (Author); Rodes, Angel (Author); Sagredo, Esteban (Author); Smedley, Rachel (Author); Smellie, John L. (Author); Thorndycraft, Varyl (Author). 2020.

Research output: Non-textual formData set/Database

E-pub ahead of print

Standard

Data for: The evolution of the Patagonian Ice Sheet from 35 ka to the Present Day (PATICE), v1. Davies, Bethan (Author); Darvill, Christopher (Author); Lovell, Harold (Author); Bendle, Jacob (Author); Dowdeswell, Julian A. (Author); Fabel, Derek (Author); Garcia, Juan-Luis (Author); Geiger, Alessa (Author); Glasser, Neil F. (Author); Gheorghiu, Delia (Author); Harrison, Stephan (Author); Hein, Andrew S. (Author); Kaplan, Michael (Author); Martin, Julian (Author); Mendelova, Monika (Author); Palmer, Adrian (Author); Pelto, Mauri (Author); Rodes, Angel (Author); Sagredo, Esteban (Author); Smedley, Rachel (Author); Smellie, John L. (Author); Thorndycraft, Varyl (Author). 2020.

Research output: Non-textual formData set/Database

Harvard

Davies, B, Darvill, C, Lovell, H, Bendle, J, Dowdeswell, JA, Fabel, D, Garcia, J-L, Geiger, A, Glasser, NF, Gheorghiu, D, Harrison, S, Hein, AS, Kaplan, M, Martin, J, Mendelova, M, Palmer, A, Pelto, M, Rodes, A, Sagredo, E, Smedley, R, Smellie, JL & Thorndycraft, V, Data for: The evolution of the Patagonian Ice Sheet from 35 ka to the Present Day (PATICE), v1, 2020, Data set/Database. https://doi.org/10.17632/ztz59y79vv.1

APA

Davies, B. (Author), Darvill, C. (Author), Lovell, H. (Author), Bendle, J. (Author), Dowdeswell, J. A. (Author), Fabel, D. (Author), Garcia, J-L. (Author), Geiger, A. (Author), Glasser, N. F. (Author), Gheorghiu, D. (Author), Harrison, S. (Author), Hein, A. S. (Author), Kaplan, M. (Author), Martin, J. (Author), Mendelova, M. (Author), Palmer, A. (Author), Pelto, M. (Author), Rodes, A. (Author), Sagredo, E. (Author), ... Thorndycraft, V. (Author). (2020). Data for: The evolution of the Patagonian Ice Sheet from 35 ka to the Present Day (PATICE), v1. Data set/Database https://doi.org/10.17632/ztz59y79vv.1

Vancouver

Author

Davies, Bethan (Author) ; Darvill, Christopher (Author) ; Lovell, Harold (Author) ; Bendle, Jacob (Author) ; Dowdeswell, Julian A. (Author) ; Fabel, Derek (Author) ; Garcia, Juan-Luis (Author) ; Geiger, Alessa (Author) ; Glasser, Neil F. (Author) ; Gheorghiu, Delia (Author) ; Harrison, Stephan (Author) ; Hein, Andrew S. (Author) ; Kaplan, Michael (Author) ; Martin, Julian (Author) ; Mendelova, Monika (Author) ; Palmer, Adrian (Author) ; Pelto, Mauri (Author) ; Rodes, Angel (Author) ; Sagredo, Esteban (Author) ; Smedley, Rachel (Author) ; Smellie, John L. (Author) ; Thorndycraft, Varyl (Author). / Data for: The evolution of the Patagonian Ice Sheet from 35 ka to the Present Day (PATICE), v1. [Data set/Database].

BibTeX

@misc{c1af6112a9d840f0a22b82287f4e7280,
title = "Data for: The evolution of the Patagonian Ice Sheet from 35 ka to the Present Day (PATICE), v1",
abstract = "We present PATICE, a GIS database of Patagonian glacial geomorphology and recalibrated chronostratigraphic data. PATICE includes 58,823 landforms and 1,669 geochronological ages, and extends from 38°S to 55°S in southern South America. We use these data to generate new empirical reconstructions of the Patagonian Ice Sheet (PIS) and subsequent ice masses and ice-dammed palaeolakes at 35 ka, 30 ka, 25 ka, 20 ka, 15 ka, 13 ka (synchronous with the Antarctic Cold Reversal), 10 ka, 5 ka, 0.2 ka and 2011 AD. At 35 ka, the PIS covered of 492.6 x103 km2, had a sea level equivalent of ~1,496 mm, was 350 km wide and 2090 km long, and was grounded on the Pacific continental shelf edge. Outlet glacier lobes remained topographically confined and the largest generated the suites of subglacial streamlined bedforms characteristic of ice streams. The PIS reached its maximum extent by 33 – 28 ka from 38°S to 48°S, and earlier, around 47 ka from 48°S southwards. Net retreat from maximum positions began by 25 ka, with ice-marginal stabilisation then at 21 – 18 ka, which was then followed by rapid irreversible deglaciation. By 15 ka, the PIS had separated into disparate ice masses, draining into large ice-dammed lakes along the eastern margin, which strongly influenced rates of recession. Glacial readvances or stabilisations occurred at least at 14 – 13 ka, 11 ka, 6 – 5 ka, 2 – 1 ka, and 0.5 – 0.2 ka. We suggest that 20th century glacial recession (% a-1) is occurring faster than at any time documented during the Holocene. ",
author = "Bethan Davies and Christopher Darvill and Harold Lovell and Jacob Bendle and Dowdeswell, {Julian A.} and Derek Fabel and Juan-Luis Garcia and Alessa Geiger and Glasser, {Neil F.} and Delia Gheorghiu and Stephan Harrison and Hein, {Andrew S.} and Michael Kaplan and Julian Martin and Monika Mendelova and Adrian Palmer and Mauri Pelto and Angel Rodes and Esteban Sagredo and Rachel Smedley and Smellie, {John L.} and Varyl Thorndycraft",
year = "2020",
month = mar,
day = "18",
doi = "http://dx.doi.org/10.17632/ztz59y79vv.1",
language = "English",

}

RIS

TY - ADVS

T1 - Data for: The evolution of the Patagonian Ice Sheet from 35 ka to the Present Day (PATICE), v1

AU - Davies, Bethan

AU - Darvill, Christopher

AU - Lovell, Harold

AU - Bendle, Jacob

AU - Dowdeswell, Julian A.

AU - Fabel, Derek

AU - Garcia, Juan-Luis

AU - Geiger, Alessa

AU - Glasser, Neil F.

AU - Gheorghiu, Delia

AU - Harrison, Stephan

AU - Hein, Andrew S.

AU - Kaplan, Michael

AU - Martin, Julian

AU - Mendelova, Monika

AU - Palmer, Adrian

AU - Pelto, Mauri

AU - Rodes, Angel

AU - Sagredo, Esteban

AU - Smedley, Rachel

AU - Smellie, John L.

AU - Thorndycraft, Varyl

PY - 2020/3/18

Y1 - 2020/3/18

N2 - We present PATICE, a GIS database of Patagonian glacial geomorphology and recalibrated chronostratigraphic data. PATICE includes 58,823 landforms and 1,669 geochronological ages, and extends from 38°S to 55°S in southern South America. We use these data to generate new empirical reconstructions of the Patagonian Ice Sheet (PIS) and subsequent ice masses and ice-dammed palaeolakes at 35 ka, 30 ka, 25 ka, 20 ka, 15 ka, 13 ka (synchronous with the Antarctic Cold Reversal), 10 ka, 5 ka, 0.2 ka and 2011 AD. At 35 ka, the PIS covered of 492.6 x103 km2, had a sea level equivalent of ~1,496 mm, was 350 km wide and 2090 km long, and was grounded on the Pacific continental shelf edge. Outlet glacier lobes remained topographically confined and the largest generated the suites of subglacial streamlined bedforms characteristic of ice streams. The PIS reached its maximum extent by 33 – 28 ka from 38°S to 48°S, and earlier, around 47 ka from 48°S southwards. Net retreat from maximum positions began by 25 ka, with ice-marginal stabilisation then at 21 – 18 ka, which was then followed by rapid irreversible deglaciation. By 15 ka, the PIS had separated into disparate ice masses, draining into large ice-dammed lakes along the eastern margin, which strongly influenced rates of recession. Glacial readvances or stabilisations occurred at least at 14 – 13 ka, 11 ka, 6 – 5 ka, 2 – 1 ka, and 0.5 – 0.2 ka. We suggest that 20th century glacial recession (% a-1) is occurring faster than at any time documented during the Holocene.

AB - We present PATICE, a GIS database of Patagonian glacial geomorphology and recalibrated chronostratigraphic data. PATICE includes 58,823 landforms and 1,669 geochronological ages, and extends from 38°S to 55°S in southern South America. We use these data to generate new empirical reconstructions of the Patagonian Ice Sheet (PIS) and subsequent ice masses and ice-dammed palaeolakes at 35 ka, 30 ka, 25 ka, 20 ka, 15 ka, 13 ka (synchronous with the Antarctic Cold Reversal), 10 ka, 5 ka, 0.2 ka and 2011 AD. At 35 ka, the PIS covered of 492.6 x103 km2, had a sea level equivalent of ~1,496 mm, was 350 km wide and 2090 km long, and was grounded on the Pacific continental shelf edge. Outlet glacier lobes remained topographically confined and the largest generated the suites of subglacial streamlined bedforms characteristic of ice streams. The PIS reached its maximum extent by 33 – 28 ka from 38°S to 48°S, and earlier, around 47 ka from 48°S southwards. Net retreat from maximum positions began by 25 ka, with ice-marginal stabilisation then at 21 – 18 ka, which was then followed by rapid irreversible deglaciation. By 15 ka, the PIS had separated into disparate ice masses, draining into large ice-dammed lakes along the eastern margin, which strongly influenced rates of recession. Glacial readvances or stabilisations occurred at least at 14 – 13 ka, 11 ka, 6 – 5 ka, 2 – 1 ka, and 0.5 – 0.2 ka. We suggest that 20th century glacial recession (% a-1) is occurring faster than at any time documented during the Holocene.

U2 - http://dx.doi.org/10.17632/ztz59y79vv.1

DO - http://dx.doi.org/10.17632/ztz59y79vv.1

M3 - Data set/Database

ER -