ABSTRACT Quantifying Climate Change: Bayesian Model for Antarctic Surface Mass Balance

Because of the importance of Antarctic surface mass balance (SMB) in predicting sea level change, models are created to predict SMB on the Antarctic ice sheet. Using Favier et al.’s quality-controlled aggregate data set N = 3529, a fully Bayesian spatial model has been utilized to predict Antarctic...

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Main Author: Philip Andrew White
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2014
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.636.4675
http://www.physics.byu.edu/docs/thesis/397/
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.636.4675 2023-05-15T13:38:43+02:00 ABSTRACT Quantifying Climate Change: Bayesian Model for Antarctic Surface Mass Balance Philip Andrew White The Pennsylvania State University CiteSeerX Archives 2014 http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.636.4675 http://www.physics.byu.edu/docs/thesis/397/ en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.636.4675 http://www.physics.byu.edu/docs/thesis/397/ Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.physics.byu.edu/docs/thesis/397/ Bayesian statistics climate modeling Gaussian process global warming Metropolis- Hastings spatial statistics surface mass balance text 2014 ftciteseerx 2016-01-08T15:43:24Z Because of the importance of Antarctic surface mass balance (SMB) in predicting sea level change, models are created to predict SMB on the Antarctic ice sheet. Using Favier et al.’s quality-controlled aggregate data set N = 3529, a fully Bayesian spatial model has been utilized to predict Antarctic SMB (Favier et al. 2013). Utilizing Markov random fields constructed through Gaussian process models, SMB is predicted over the entire Antarctic ice sheet. An SMB surface over the Antarctic ice sheet is computed by this model and compared with previous maps. An SMB predic-tion error surface is created to identify regions of high prediction uncertainty. This model estimates total SMB to be 1.75±0.335 ·1012 m3 ·w.e ·yr−1 and mean SMB as 124.80±23.85 mm ·w.e. ·yr−1. These results suggest lower Antarctic water accumulation than previously purported. The calcu-lated SMB surface showed more negative SMB regions and higher spatial variation than is likely plausible. Lastly, Antarctic boundary regions and areas with little data show high prediction un-certainty by the generated SMB prediction uncertainty surface. Text Antarc* Antarctic Ice Sheet Unknown Antarctic Hastings ENVELOPE(-154.167,-154.167,-85.567,-85.567) The Antarctic
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Bayesian statistics
climate modeling
Gaussian process
global warming
Metropolis- Hastings
spatial statistics
surface mass balance
spellingShingle Bayesian statistics
climate modeling
Gaussian process
global warming
Metropolis- Hastings
spatial statistics
surface mass balance
Philip Andrew White
ABSTRACT Quantifying Climate Change: Bayesian Model for Antarctic Surface Mass Balance
topic_facet Bayesian statistics
climate modeling
Gaussian process
global warming
Metropolis- Hastings
spatial statistics
surface mass balance
description Because of the importance of Antarctic surface mass balance (SMB) in predicting sea level change, models are created to predict SMB on the Antarctic ice sheet. Using Favier et al.’s quality-controlled aggregate data set N = 3529, a fully Bayesian spatial model has been utilized to predict Antarctic SMB (Favier et al. 2013). Utilizing Markov random fields constructed through Gaussian process models, SMB is predicted over the entire Antarctic ice sheet. An SMB surface over the Antarctic ice sheet is computed by this model and compared with previous maps. An SMB predic-tion error surface is created to identify regions of high prediction uncertainty. This model estimates total SMB to be 1.75±0.335 ·1012 m3 ·w.e ·yr−1 and mean SMB as 124.80±23.85 mm ·w.e. ·yr−1. These results suggest lower Antarctic water accumulation than previously purported. The calcu-lated SMB surface showed more negative SMB regions and higher spatial variation than is likely plausible. Lastly, Antarctic boundary regions and areas with little data show high prediction un-certainty by the generated SMB prediction uncertainty surface.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Philip Andrew White
author_facet Philip Andrew White
author_sort Philip Andrew White
title ABSTRACT Quantifying Climate Change: Bayesian Model for Antarctic Surface Mass Balance
title_short ABSTRACT Quantifying Climate Change: Bayesian Model for Antarctic Surface Mass Balance
title_full ABSTRACT Quantifying Climate Change: Bayesian Model for Antarctic Surface Mass Balance
title_fullStr ABSTRACT Quantifying Climate Change: Bayesian Model for Antarctic Surface Mass Balance
title_full_unstemmed ABSTRACT Quantifying Climate Change: Bayesian Model for Antarctic Surface Mass Balance
title_sort abstract quantifying climate change: bayesian model for antarctic surface mass balance
publishDate 2014
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.636.4675
http://www.physics.byu.edu/docs/thesis/397/
long_lat ENVELOPE(-154.167,-154.167,-85.567,-85.567)
geographic Antarctic
Hastings
The Antarctic
geographic_facet Antarctic
Hastings
The Antarctic
genre Antarc*
Antarctic
Ice Sheet
genre_facet Antarc*
Antarctic
Ice Sheet
op_source http://www.physics.byu.edu/docs/thesis/397/
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.636.4675
http://www.physics.byu.edu/docs/thesis/397/
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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