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Local Warming

Author(s): Vanderbei, Robert J.

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dc.contributor.authorVanderbei, Robert J.-
dc.date.accessioned2016-10-17T14:13:38Z-
dc.date.available2016-10-17T14:13:38Z-
dc.date.issued2012-01en_US
dc.identifier.citationVanderbei, Robert J. "Local Warming" SIAM Review, 54(3), 597 - 606, 2012. doi:10.1137/110827296en_US
dc.identifier.issn0036-1445-
dc.identifier.urihttp://arks.princeton.edu/ark:/88435/pr16w2g-
dc.description.abstractUsing 55 years of daily average temperatures from a local weather station, I made a least-absolute-deviations (LAD) regression model that accounts for three effects: seasonal variations, the 11-year solar cycle, and a linear trend. The model was formulated as a linear programming problem and solved using widely available optimization software. The solution indicates that temperatures have gone up by about $2^\circ \mbox{F}$ over the 55 years covered by the data. It also correctly identifies the known phase of the solar cycle; i.e., the date of the last solar minimum. It turns out that the maximum slope of the solar cycle sinusoid in the regression model is about the same size as the slope produced by the linear trend. The fact that the solar cycle was correctly extracted by the model is a strong indicator that effects of this size, in particular the slope of the linear trend, can be accurately determined from the 55 years of data analyzed. The main purpose for doing this analysis is to demonstrate that it is easy to find and analyze archived temperature data for oneself. In particular, this problem makes a good class project for upper-level undergraduate courses in optimization or in statistics. It is worth noting that a similar least-squares model failed to characterize the solar cycle correctly, and hence even though it too indicates that temperatures have been rising locally, one can be less confident in this result. The paper ends with a section presenting similar results from a few thousand sites distributed worldwide, some results from a modification of the model that includes both temperature and humidity, as well as a number of suggestions for future work and/or ideas for enhancements that could be used as classroom projects.en_US
dc.format.extent597 - 606en_US
dc.relation.ispartofSIAM Reviewen_US
dc.rightsThis is the publisher’s version of the article (version of record). All rights reserved to the publisher. Please refer to the publisher's site for terms of use.en_US
dc.titleLocal Warmingen_US
dc.typeJournal Articleen_US
dc.identifier.doidoi:10.1137/110827296-
dc.identifier.eissn1095-7200-

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