On multi-timescale variability of temperature in China in modulated annual cycle reference frame

The traditional anomaly (TA) reference frame and its corresponding anomaly for a given data span changes with the extension of data length. In this study, the modulated annual cycle (MAC), instead of the widely used climatological mean annual cycle, is used as an alternative reference frame for computing climate anomalies to study the multi-timescale variability of surface air temperature (SAT) in China based on homogenized daily data from 1952 to 2004. The Ensemble Empirical Mode Decomposition (EEMD) method is used to separate daily SAT into a high frequency component, a MAC component, an interannual component, and a decadal-to-trend component. The results show that the EEMD method can reflect historical events reasonably well, indicating its adaptive and temporally local characteristics. It is shown that MAC is a temporally local reference frame and will not be altered over a particular time span by an extension of data length, thereby making it easier for physical interpretation. In the MAC reference frame, the low frequency component is found more suitable for studying the interannual to longer timescale variability (ILV) than a 13-month window running mean, which does not exclude the annual cycle. It is also better than other traditional versions (annual or summer or winter mean) of ILV, which contains a portion of the annual cycle. The analysis reveals that the variability of the annual cycle could be as large as the magnitude of interannual variability. The possible physical causes of different timescale variability of SAT in China are further discussed.

[1]  Bin Wang,et al.  A review on aspects of climate simulation assessment , 2009 .

[2]  H. L. Miller,et al.  Climate Change 2007: The Physical Science Basis , 2007 .

[3]  Wang Lin Interannual Variations of Winter Temperature in China and Their Relationship with the Atmospheric Circulation and Sea Surface Temperature , 2009 .

[4]  N. Huang,et al.  The empirical mode decomposition and the Hilbert spectrum for nonlinear and non-stationary time series analysis , 1998, Proceedings of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences.

[5]  T. Zhou,et al.  Impacts of winter‐NAO on March cooling trends over subtropical Eurasia continent in the recent half century , 2004 .

[6]  Tianjun Zhou,et al.  Twentieth-Century Surface Air Temperature over China and the Globe Simulated by Coupled Climate Models , 2006 .

[7]  Gabriel Rilling,et al.  Empirical mode decomposition as a filter bank , 2004, IEEE Signal Processing Letters.

[8]  Zhaojian Zong Attribution of the 20th Century Climate Warming in China , 2005 .

[9]  王文,et al.  STUDIES ON CLIMATE CHANGE IN CHINA IN RECENT 45 YEARS , 1998 .

[10]  W. Collins,et al.  The NCEP–NCAR 50-Year Reanalysis: Monthly Means CD-ROM and Documentation , 2001 .

[11]  Zhu Yimin,et al.  Relationships between Pacific Decadal Oscillation and climate variabilities in China , 2003 .

[12]  Tianjun Zhou,et al.  Detecting and understanding the multi-decadal variability of the East Asian Summer Monsoon: Recent progress and state of affairs , 2009 .

[13]  David B. Stephenson,et al.  The Variability of Seasonality , 2005 .

[14]  Zhongwei Yan,et al.  On the secular change of spring onset at Stockholm , 2009 .

[15]  Zhaohua Wu,et al.  On the trend, detrending, and variability of nonlinear and nonstationary time series , 2007, Proceedings of the National Academy of Sciences.

[16]  S. S. Shen,et al.  A confidence limit for the empirical mode decomposition and Hilbert spectral analysis , 2003, Proceedings of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences.

[17]  R. Reynolds,et al.  The NCEP/NCAR 40-Year Reanalysis Project , 1996, Renewable Energy.

[18]  N. Huang,et al.  A new view of nonlinear water waves: the Hilbert spectrum , 1999 .

[19]  Consistence and Inconsistence of Variations in Surface Air Temperatures between Eastern and Western China during 1951~2002 , 2005 .

[20]  Thomas M. Smith,et al.  Interdecadal Changes of 30-Yr SST Normals during 1871–2000 , 2003 .

[21]  T. Zhou,et al.  Seasonality and Three-Dimensional Structure of Interdecadal Change in the East Asian Monsoon , 2007 .

[22]  N. Huang,et al.  A study of the characteristics of white noise using the empirical mode decomposition method , 2004, Proceedings of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences.

[23]  Norden E. Huang,et al.  Ensemble Empirical Mode Decomposition: a Noise-Assisted Data Analysis Method , 2009, Adv. Data Sci. Adapt. Anal..

[24]  Norden E. Huang,et al.  A review on Hilbert‐Huang transform: Method and its applications to geophysical studies , 2008 .

[25]  Zeng‐Zhen Hu,et al.  Summer climate variability in China and its association with 500 hPa height and tropical convection. , 1996 .

[26]  P. Jones,et al.  A MAINLAND CHINA HOMOgENIZED HISTORICAL TEMPERATURE DATASET Of 1951-2004 , 2009 .

[27]  P PamelaSwain,et al.  A new view , 2004 .

[28]  Diane Foucar-Szocki,et al.  A New View , 1993 .

[29]  Swadhin K. Behera,et al.  El Niño Modoki and its possible teleconnection , 2007 .

[30]  Hans W. Linderholm,et al.  Growing season changes in the last century , 2006 .

[31]  Lin Zhen-shan The Regional Features of Temperature Variation Trends over China by Empirical Mode Decomposition Method , 2007 .

[32]  W. Shaowu,et al.  Influence of Arctic Oscillation on winter climate over China , 2003 .

[33]  Song Yang,et al.  Long‐term climate variations in China and global warming signals , 2003 .

[34]  C. Tucker,et al.  The modulated annual cycle: an alternative reference frame for climate anomalies , 2007 .

[35]  Norden E. Huang,et al.  HHT ANALYSIS OF THE NONLINEAR AND NON-STATIONARY ANNUAL CYCLE OF DAILY SURFACE AIR TEMPERATURE DATA , 2010 .

[36]  Zhang De,et al.  National Assessment Report of Climate Change (I): Climate change in China and its future trend , 2006 .

[37]  Shaowu Wang,et al.  Interdecadal variability of temperature and precipitation in China since 1880 , 2004 .