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The DOI matches its Crossref record; 23 of the 23 references it cites were found in a registry or an index.

Evolution of land surface air temperature trend

Open access
Ji, Fei, Wu, Zhaohua, Huang, Jianping, Chassignet, Eric P.·2014·Nature Climate Change

Abstract

The global climate has been experiencing significant warming at an unprecedented pace in the past century(1,2). This warming is spatially and temporally non-uniform, and one needs to understand its evolution to better evaluate its potential societal and economic impact. Here, the evolution of global land surface air temperature trend in the past century is diagnosed using the spatial-temporally multidimensional ensemble empirical mode decomposition method(3). We find that the noticeable warming (>0.5 K) started sporadically over the global land and accelerated until around 1980. Both the warming rate and spatial structure have changed little since. The fastest warming in recent decades (>0.4 K per decade) occurred in northern mid-latitudes. From a zonal average perspective, noticeable warming (>0.2 K since 1900) first took place in the subtropical and subpolar regions of the Northern Hemisphere, followed by subtropical warming in the Southern Hemisphere. The two bands of warming in the Northern Hemisphere expanded from 1950 to 1985 and merged to cover the entire Northern Hemisphere.

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Cites

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Research works printed but not linked: 7

  1. Wu, Z., Huang, N. E. & Chen, X. The multi-dimensional ensemble empirical mode decomposition method. Adv. Adapt. Data Anal. 1, 339–372 (2009). · doi:10.1142/s1793536909000187
  2. Franzke, C. Multi-scale analysis of teleconnection indices: Climate noise and nonlinear trends analysis. Nonlinear Proc. Geoph. 16, 65–76 (2009). · doi:10.5194/npg-16-65-2009
  3. Ruzmaikin, A. & Feynman, J. Search for climate trends in satellite data. Adv. Adapt. Data Anal. 1, 667–679 (2009). · doi:10.1142/s1793536909000266
  4. Franzke, C. & Woollings, T. On the persistence and predictability properties of North Atlantic climate variability. J. Clim. 24, 466–472 (2011). · doi:10.1175/2010jcli3739.1
  5. Hu, Z. Z., Huang, B., Kinter, J. L. III, Wu, Z. & Kumar, A. Connection of the stratospheric QBO with global atmospheric general circulation and tropical SST Part II: Interdecadal variations. Clim. Dynam. 38, 25–43 (2012). · doi:10.1007/s00382-011-1073-6
  6. Huang, B. et al. Influences of subtropical air–sea interaction on the multidecadal AMOC variability in the NCEP climate forecast system. Clim. Dynam. 39, 631–555 (2012).
  7. Hudson, R. D., Andrade, M. F., Follette, M. B. & Frolov, A. D. The total ozone field separated into meteorological regimes–Part II: Northern Hemisphere mid-latitude total ozone trends. Atmos. Chem. Phys. 6, 5183–5191 (2006). · doi:10.5194/acp-6-5183-2006

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Metadata

Authors
Ji, F., Wu, Z., Huang, J., & Chassignet, E. P.
Venue
Nature Climate Change
Published
2014-05-04
Volume
4
Issue
6
Pages
462-466
ISSN
  • 1758-678X (ISSN-L)
  • 1758-6798
OpenAlex
W2083808131
Cited by
601
References
23
FWCI
36.09
Type
journal article
Language
en
Open access
green
Licence
www.springer.com/tdm (tdm)

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Ji, F., Wu, Z., Huang, J., & Chassignet, E. P. (2014). Evolution of land surface air temperature trend. Nature Climate Change. https://doi.org/10.1038/nclimate2223

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