Separation of melting and environmental signals in an ice core with seasonal melt

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Standard

Separation of melting and environmental signals in an ice core with seasonal melt. / Moore, J C; Grinsted, Aslak; Kekonen, T; Pohjola, V.

In: Geophysical Research Letters, Vol. 32, No. L10501, 2005.

Research output: Contribution to journal › Journal article › Research › peer-review

Harvard

Moore, JC, Grinsted, A, Kekonen, T & Pohjola, V 2005, 'Separation of melting and environmental signals in an ice core with seasonal melt', Geophysical Research Letters, vol. 32, no. L10501.

APA

Moore, J. C., Grinsted, A., Kekonen, T., & Pohjola, V. (2005). Separation of melting and environmental signals in an ice core with seasonal melt. Geophysical Research Letters, 32(L10501).

Vancouver

Moore JC, Grinsted A, Kekonen T, Pohjola V. Separation of melting and environmental signals in an ice core with seasonal melt. Geophysical Research Letters. 2005;32(L10501).

Author

Moore, J C ; Grinsted, Aslak ; Kekonen, T ; Pohjola, V. / Separation of melting and environmental signals in an ice core with seasonal melt. In: Geophysical Research Letters. 2005 ; Vol. 32, No. L10501.

Bibtex

@article{94427b30e62b11ddbf70000ea68e967b,
title = "Separation of melting and environmental signals in an ice core with seasonal melt",
abstract = "We examine the impact of melt water percolation on the soluble ion chemical record from the Lomonosovfonna ice core. Principle component analysis shows that melting produces only simple changes between bubbly and clear ice facies, due to elution of ions. The data can be naturally split into four groups: pre-industrial, immediately before, and after the end of the Little Ice Age, and anthropogenic impact eras. The 2nd, 3rd and 4th principle components for these periods all differ significantly, reflecting complex changes in environmental conditions. Thus the core preserves a rich record of environmental history, and simple one of melting. We construct a model of percolation effects to reconstruct “pristine” ice chemical composition, finding that even with melt percentages as high as 80%, there is little disturbance to the chemical stratigraphy. This suggests that ionic records from Arctic ice cap cores are nearly as reliable as those from Greenland or Antarctica.",
author = "Moore, {J C} and Aslak Grinsted and T Kekonen and V Pohjola",
note = "Paper id:: 10.1029/2005GL023039",
year = "2005",
language = "English",
volume = "32",
journal = "Geophysical Research Letters",
issn = "0094-8276",
publisher = "Wiley-Blackwell",
number = "L10501",

}

RIS

TY - JOUR

T1 - Separation of melting and environmental signals in an ice core with seasonal melt

AU - Moore, J C

AU - Grinsted, Aslak

AU - Kekonen, T

AU - Pohjola, V

N1 - Paper id:: 10.1029/2005GL023039

PY - 2005

Y1 - 2005

N2 - We examine the impact of melt water percolation on the soluble ion chemical record from the Lomonosovfonna ice core. Principle component analysis shows that melting produces only simple changes between bubbly and clear ice facies, due to elution of ions. The data can be naturally split into four groups: pre-industrial, immediately before, and after the end of the Little Ice Age, and anthropogenic impact eras. The 2nd, 3rd and 4th principle components for these periods all differ significantly, reflecting complex changes in environmental conditions. Thus the core preserves a rich record of environmental history, and simple one of melting. We construct a model of percolation effects to reconstruct “pristine” ice chemical composition, finding that even with melt percentages as high as 80%, there is little disturbance to the chemical stratigraphy. This suggests that ionic records from Arctic ice cap cores are nearly as reliable as those from Greenland or Antarctica.

AB - We examine the impact of melt water percolation on the soluble ion chemical record from the Lomonosovfonna ice core. Principle component analysis shows that melting produces only simple changes between bubbly and clear ice facies, due to elution of ions. The data can be naturally split into four groups: pre-industrial, immediately before, and after the end of the Little Ice Age, and anthropogenic impact eras. The 2nd, 3rd and 4th principle components for these periods all differ significantly, reflecting complex changes in environmental conditions. Thus the core preserves a rich record of environmental history, and simple one of melting. We construct a model of percolation effects to reconstruct “pristine” ice chemical composition, finding that even with melt percentages as high as 80%, there is little disturbance to the chemical stratigraphy. This suggests that ionic records from Arctic ice cap cores are nearly as reliable as those from Greenland or Antarctica.

M3 - Journal article

VL - 32

JO - Geophysical Research Letters

JF - Geophysical Research Letters

SN - 0094-8276

IS - L10501

ER -

ID: 9832578