Climate and Dynamics
Break detection of annual Swiss temperature series
Article first published online: 4 JUL 2012
DOI: 10.1029/2012JD017729
©2012. American Geophysical Union. All Rights Reserved.
Additional Information
How to Cite
, , , , , and (2012), Break detection of annual Swiss temperature series, J. Geophys. Res., 117, D13105, doi:10.1029/2012JD017729.
Publication History
- Issue published online: 4 JUL 2012
- Article first published online: 4 JUL 2012
- Manuscript Accepted: 29 MAY 2012
- Manuscript Revised: 25 MAY 2012
- Manuscript Received: 4 MAR 2012
Keywords:
- Switzerland;
- break detection;
- climate data homogenization;
- instrumental climate data;
- weather station history
[1] Instrumental temperature series are often affected by artificial breaks (“break points”) due to (e.g.,) changes in station location, land-use, or instrumentation. The Swiss climate observation network offers a high number and density of stations, many long and relatively complete daily to sub-daily temperature series, and well-documented station histories (i.e., metadata). However, for many climate observation networks outside of Switzerland, detailed station histories are missing, incomplete, or inaccessible. To correct these records, the use of reliable statistical break detection methods is necessary. Here, we apply three statistical break detection methods to high-quality Swiss temperature series and use the available metadata to assess the methods. Due to the complex terrain in Switzerland, we are able to assess these methods under specific local conditions such as the Foehn or crest situations. We find that the temperature series of all stations are affected by artificial breaks (average = 1 break point / 48 years) with discrepancies in the abilities of the methods to detect breaks. However, by combining the three statistical methods, almost all of the detected break points are confirmed by metadata. In most cases, these break points are ascribed to a combination of factors in the station history.

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