Explicit solutions for a probabilistic moraine preservation model
If a series of glacial advances occurs over the same pathway, the moraines that are now present may constitute an incomplete record of the total history. This is because a given advance can destroy the moraine left by a previous one, if the previous advance was less extensive. Gibbons, Megeath and P...
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ftdoajarticles:oai:doaj.org/article:8e915d6ab1284549b11381f7abe73a01 2023-05-15T16:57:35+02:00 Explicit solutions for a probabilistic moraine preservation model PAUL MUZIKAR 2016-12-01T00:00:00Z https://doi.org/10.1017/jog.2016.109 https://doaj.org/article/8e915d6ab1284549b11381f7abe73a01 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S002214301600109X/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2016.109 0022-1430 1727-5652 https://doaj.org/article/8e915d6ab1284549b11381f7abe73a01 Journal of Glaciology, Vol 62, Pp 1181-1185 (2016) glaciation moraines stochastic model Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2016 ftdoajarticles https://doi.org/10.1017/jog.2016.109 2023-03-12T01:30:59Z If a series of glacial advances occurs over the same pathway, the moraines that are now present may constitute an incomplete record of the total history. This is because a given advance can destroy the moraine left by a previous one, if the previous advance was less extensive. Gibbons, Megeath and Pierce (GMP) formulated an elegant stochastic model for this process; the key quantity in their analysis is $\bi P(n\vert N)$ , the probability that n moraines are preserved after N glacial advances. In their paper, GMP derive a recursion formula satisfied by $\bi P(n\vert N)$ , and use this formula to compute values of P for a range of values of n and N. In the present paper, we derive an explicit general answer for $\bi P(n\vert N)$ , and show explicit, exact results for the mean value and standard deviation of n. We use these results to develop more insight into the consequences of the GMP model; for example, to a good approximation, 〈n〉 increases as ln(N). We explain how a Bayesian approach can be used to analyze $\bi P(N\vert n)$ , the probability that there were N advances, given that we now observe n moraines. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 62 236 1181 1185 |
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Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
glaciation moraines stochastic model Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
glaciation moraines stochastic model Environmental sciences GE1-350 Meteorology. Climatology QC851-999 PAUL MUZIKAR Explicit solutions for a probabilistic moraine preservation model |
topic_facet |
glaciation moraines stochastic model Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
If a series of glacial advances occurs over the same pathway, the moraines that are now present may constitute an incomplete record of the total history. This is because a given advance can destroy the moraine left by a previous one, if the previous advance was less extensive. Gibbons, Megeath and Pierce (GMP) formulated an elegant stochastic model for this process; the key quantity in their analysis is $\bi P(n\vert N)$ , the probability that n moraines are preserved after N glacial advances. In their paper, GMP derive a recursion formula satisfied by $\bi P(n\vert N)$ , and use this formula to compute values of P for a range of values of n and N. In the present paper, we derive an explicit general answer for $\bi P(n\vert N)$ , and show explicit, exact results for the mean value and standard deviation of n. We use these results to develop more insight into the consequences of the GMP model; for example, to a good approximation, 〈n〉 increases as ln(N). We explain how a Bayesian approach can be used to analyze $\bi P(N\vert n)$ , the probability that there were N advances, given that we now observe n moraines. |
format |
Article in Journal/Newspaper |
author |
PAUL MUZIKAR |
author_facet |
PAUL MUZIKAR |
author_sort |
PAUL MUZIKAR |
title |
Explicit solutions for a probabilistic moraine preservation model |
title_short |
Explicit solutions for a probabilistic moraine preservation model |
title_full |
Explicit solutions for a probabilistic moraine preservation model |
title_fullStr |
Explicit solutions for a probabilistic moraine preservation model |
title_full_unstemmed |
Explicit solutions for a probabilistic moraine preservation model |
title_sort |
explicit solutions for a probabilistic moraine preservation model |
publisher |
Cambridge University Press |
publishDate |
2016 |
url |
https://doi.org/10.1017/jog.2016.109 https://doaj.org/article/8e915d6ab1284549b11381f7abe73a01 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology, Vol 62, Pp 1181-1185 (2016) |
op_relation |
https://www.cambridge.org/core/product/identifier/S002214301600109X/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2016.109 0022-1430 1727-5652 https://doaj.org/article/8e915d6ab1284549b11381f7abe73a01 |
op_doi |
https://doi.org/10.1017/jog.2016.109 |
container_title |
Journal of Glaciology |
container_volume |
62 |
container_issue |
236 |
container_start_page |
1181 |
op_container_end_page |
1185 |
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1766049145222594560 |