Coastal atmospheric temperature prediction in Greenland using support vector regression

In the recent years, global climate change has induced evergrowing loss of sea ice in the Arctic. As the sea ice disappears, albedo diminishes and the sea surface is more likely to be warmed by incoming solar radiation. With the right wind conditions, this extra heat may also be advected towards the...

Full description

Bibliographic Details
Main Author: Parkan, Matthew Josef
Format: Text
Language:unknown
Published: 2014
Subjects:
Online Access:http://infoscience.epfl.ch/record/196280
https://infoscience.epfl.ch/record/196280/files/Master_Thesis_Parkan_2012.pdf
id ftinfoscience:oai:infoscience.tind.io:196280
record_format openpolar
spelling ftinfoscience:oai:infoscience.tind.io:196280 2023-12-24T10:07:48+01:00 Coastal atmospheric temperature prediction in Greenland using support vector regression Parkan, Matthew Josef 2014-01-27T08:11:27Z http://infoscience.epfl.ch/record/196280 https://infoscience.epfl.ch/record/196280/files/Master_Thesis_Parkan_2012.pdf unknown http://infoscience.epfl.ch/record/196280 https://infoscience.epfl.ch/record/196280/files/Master_Thesis_Parkan_2012.pdf http://infoscience.epfl.ch/record/196280 Text 2014 ftinfoscience 2023-11-27T00:51:14Z In the recent years, global climate change has induced evergrowing loss of sea ice in the Arctic. As the sea ice disappears, albedo diminishes and the sea surface is more likely to be warmed by incoming solar radiation. With the right wind conditions, this extra heat may also be advected towards the shore and thus influence coastal atmospheric temperatures. Thus, knowing how coastal atmospheric temperature is related to offshore conditions is paramount to help predict inshore effects. To study this relation, an exploratory approach using machine learning algorithms is proposed. Based on a combination of daily in situ (i.e. wind velocity, sea level pressure) and remotely sensed (i.e. sea surface temperature, sea ice concentration) data, a series of predicting features are constructed for the years 1981-2010. Two implementations of support vector regression (SVR), one with a linear kernel and the other with a combination of gaussian and histogram intersection kernels are then applied. Results of the SVR indicate that prediction root mean squared errors of less than 5°C are routinely achievable. Prediction errors are also found to be the smallest in summer months and/or at lower latitudes. Finally, the relative importance (ranking) of features appears to be highly variable, depending both on the location and the period of the year. Text albedo Arctic Climate change Greenland Sea ice EPFL Infoscience (Ecole Polytechnique Fédérale Lausanne) Arctic Greenland
institution Open Polar
collection EPFL Infoscience (Ecole Polytechnique Fédérale Lausanne)
op_collection_id ftinfoscience
language unknown
description In the recent years, global climate change has induced evergrowing loss of sea ice in the Arctic. As the sea ice disappears, albedo diminishes and the sea surface is more likely to be warmed by incoming solar radiation. With the right wind conditions, this extra heat may also be advected towards the shore and thus influence coastal atmospheric temperatures. Thus, knowing how coastal atmospheric temperature is related to offshore conditions is paramount to help predict inshore effects. To study this relation, an exploratory approach using machine learning algorithms is proposed. Based on a combination of daily in situ (i.e. wind velocity, sea level pressure) and remotely sensed (i.e. sea surface temperature, sea ice concentration) data, a series of predicting features are constructed for the years 1981-2010. Two implementations of support vector regression (SVR), one with a linear kernel and the other with a combination of gaussian and histogram intersection kernels are then applied. Results of the SVR indicate that prediction root mean squared errors of less than 5°C are routinely achievable. Prediction errors are also found to be the smallest in summer months and/or at lower latitudes. Finally, the relative importance (ranking) of features appears to be highly variable, depending both on the location and the period of the year.
format Text
author Parkan, Matthew Josef
spellingShingle Parkan, Matthew Josef
Coastal atmospheric temperature prediction in Greenland using support vector regression
author_facet Parkan, Matthew Josef
author_sort Parkan, Matthew Josef
title Coastal atmospheric temperature prediction in Greenland using support vector regression
title_short Coastal atmospheric temperature prediction in Greenland using support vector regression
title_full Coastal atmospheric temperature prediction in Greenland using support vector regression
title_fullStr Coastal atmospheric temperature prediction in Greenland using support vector regression
title_full_unstemmed Coastal atmospheric temperature prediction in Greenland using support vector regression
title_sort coastal atmospheric temperature prediction in greenland using support vector regression
publishDate 2014
url http://infoscience.epfl.ch/record/196280
https://infoscience.epfl.ch/record/196280/files/Master_Thesis_Parkan_2012.pdf
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre albedo
Arctic
Climate change
Greenland
Sea ice
genre_facet albedo
Arctic
Climate change
Greenland
Sea ice
op_source http://infoscience.epfl.ch/record/196280
op_relation http://infoscience.epfl.ch/record/196280
https://infoscience.epfl.ch/record/196280/files/Master_Thesis_Parkan_2012.pdf
_version_ 1786155966489690112