New Tools for Analyzing Time Series Relationships and Trends

Research output: Contribution to journalJournal articleResearchpeer-review

Standard

New Tools for Analyzing Time Series Relationships and Trends. / Moore, J C; Grinsted, Aslak; Jevrejeva, S.

In: EOS : Transactions, Vol. 86, No. 24, 2005.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Moore, JC, Grinsted, A & Jevrejeva, S 2005, 'New Tools for Analyzing Time Series Relationships and Trends', EOS : Transactions, vol. 86, no. 24.

APA

Moore, J. C., Grinsted, A., & Jevrejeva, S. (2005). New Tools for Analyzing Time Series Relationships and Trends. EOS : Transactions, 86(24).

Vancouver

Moore JC, Grinsted A, Jevrejeva S. New Tools for Analyzing Time Series Relationships and Trends. EOS : Transactions. 2005;86(24).

Author

Moore, J C ; Grinsted, Aslak ; Jevrejeva, S. / New Tools for Analyzing Time Series Relationships and Trends. In: EOS : Transactions. 2005 ; Vol. 86, No. 24.

Bibtex

@article{ec0362d0e62b11ddbf70000ea68e967b,
title = "New Tools for Analyzing Time Series Relationships and Trends",
abstract = "Geophysical studies are plagued by short and noisy time series. These time series are typically nonstationary, contain various long-period quasi-periodic components, and have rather low signal-to-noise ratios and/or poor spatial sampling. Classic examples of these time series are tide gauge records, which are influenced by ocean and atmospheric circulation patterns, twentieth-century warming, and other long-term variability. Remarkable progress recently has been made in the statistical analysis of time series. Ghil et al. [2002] presented a general review of several advanced statistical methods with a solid theoretical foundation. This present article highlights several new approaches that are easy to use and that may be of general interest. Extracting trends from data is a key element of many geophysical studies; however, when the best fit is clearly not linear, it can be difficult to evaluate appropriate errors for the trend. Here, a method is suggested of finding a data-adaptive nonlinear trend and its error at any point along the trend. The method has significant advantages over, e.g., low-pass filtering or fitting by polynomial functions in that as the fit is data adaptive, no preconceived functions are forced on the data; the errors associated with the trend are then usually much smaller than individual measurement errors.",
author = "Moore, {J C} and Aslak Grinsted and S Jevrejeva",
note = "Paper id:: 10.1029/2005EO240003",
year = "2005",
language = "English",
volume = "86",
journal = "Trans Amer Geophys Union",
issn = "0096-3941",
publisher = "AGU Publications",
number = "24",

}

RIS

TY - JOUR

T1 - New Tools for Analyzing Time Series Relationships and Trends

AU - Moore, J C

AU - Grinsted, Aslak

AU - Jevrejeva, S

N1 - Paper id:: 10.1029/2005EO240003

PY - 2005

Y1 - 2005

N2 - Geophysical studies are plagued by short and noisy time series. These time series are typically nonstationary, contain various long-period quasi-periodic components, and have rather low signal-to-noise ratios and/or poor spatial sampling. Classic examples of these time series are tide gauge records, which are influenced by ocean and atmospheric circulation patterns, twentieth-century warming, and other long-term variability. Remarkable progress recently has been made in the statistical analysis of time series. Ghil et al. [2002] presented a general review of several advanced statistical methods with a solid theoretical foundation. This present article highlights several new approaches that are easy to use and that may be of general interest. Extracting trends from data is a key element of many geophysical studies; however, when the best fit is clearly not linear, it can be difficult to evaluate appropriate errors for the trend. Here, a method is suggested of finding a data-adaptive nonlinear trend and its error at any point along the trend. The method has significant advantages over, e.g., low-pass filtering or fitting by polynomial functions in that as the fit is data adaptive, no preconceived functions are forced on the data; the errors associated with the trend are then usually much smaller than individual measurement errors.

AB - Geophysical studies are plagued by short and noisy time series. These time series are typically nonstationary, contain various long-period quasi-periodic components, and have rather low signal-to-noise ratios and/or poor spatial sampling. Classic examples of these time series are tide gauge records, which are influenced by ocean and atmospheric circulation patterns, twentieth-century warming, and other long-term variability. Remarkable progress recently has been made in the statistical analysis of time series. Ghil et al. [2002] presented a general review of several advanced statistical methods with a solid theoretical foundation. This present article highlights several new approaches that are easy to use and that may be of general interest. Extracting trends from data is a key element of many geophysical studies; however, when the best fit is clearly not linear, it can be difficult to evaluate appropriate errors for the trend. Here, a method is suggested of finding a data-adaptive nonlinear trend and its error at any point along the trend. The method has significant advantages over, e.g., low-pass filtering or fitting by polynomial functions in that as the fit is data adaptive, no preconceived functions are forced on the data; the errors associated with the trend are then usually much smaller than individual measurement errors.

M3 - Journal article

VL - 86

JO - Trans Amer Geophys Union

JF - Trans Amer Geophys Union

SN - 0096-3941

IS - 24

ER -

ID: 9832585