Abstract
Trend uncertainty in the ozone valley over the Tibetan Plateau (OVTP) and the South Asian high (SAH) during 1979–2009 in ERA-Interim (interim reanalysis data from the ECMWF), JRA-55 (55-yr reanalysis data from the Japan Meteorological Agency), and NCEP-CFSR (Climate Forecast System Reanalysis) datasets was evaluated. The results showed that the NCEP-CFSR OVTP became strong in the summers of 1979–2009, whereas it became weak according to ERA-Interim and JRA-55. Satellite data merged with TOMS (Total Ozone Mapping Spectrometer) and OMI (Ozone Monitoring Instrument) agreed with the OVTP trend of NCEP-CFSR. The OVTP strengthening in NCEP-CFSR may have been caused by SAH intensification, a rising tropopause, and increasing ozone over non-TP (non-Tibetan Plateau) areas (27°–37°N, < 75°E and > 105°E). Analogously, the OVTP weakening in ERA-Interim and JRA-55 may have been affected by weakening SAH, descending tropopause, and decreasing non-TP ozone.
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Supported by the National Natural Science Foundation of China (41305039, 41675039, 91537213, 41375047, 41375092, 41475140, 41641042, and 41575057) and Priority Academic Program Development of Jiangsu Higher Education Institutions (PAPD).
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Guo, D., Su, Y., Zhou, X. et al. Evaluation of the trend uncertainty in summer ozone valley over the Tibetan Plateau in three reanalysis datasets. J Meteorol Res 31, 431–437 (2017). https://doi.org/10.1007/s13351-017-6058-x
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DOI: https://doi.org/10.1007/s13351-017-6058-x