z-logo
Premium
Validation of eight atmospheric reanalyses in the Antarctic Peninsula region
Author(s) -
Nygård Tiina,
Vihma Timo,
Birnbaum Gerit,
Hartmann Jörg,
King John,
LachlanCope Tom,
Ladkin Russell,
Lüpkes Christof,
Weiss Alexandra
Publication year - 2015
Publication title -
quarterly journal of the royal meteorological society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.744
H-Index - 143
eISSN - 1477-870X
pISSN - 0035-9009
DOI - 10.1002/qj.2691
Subject(s) - environmental science , peninsula , wind speed , climatology , humidity , meteorology , atmospheric sciences , data assimilation , climate forecast system , geology , geography , precipitation , archaeology
Eight atmospheric reanalyses were compared against observed vertical profiles of temperature, specific humidity and wind speed collected by two research aircraft in F ebruary– M arch 2010 in the A ntarctic P eninsula region. These data offered a rare possibility to validate reanalyses against independent in situ data which have not been assimilated into the reanalyses. The reanalyses had generally too moist profiles with too low wind speeds, but otherwise the errors in the reanalyses had large spatial differences. On the eastern side of the peninsula, the near‐surface temperatures were largely overestimated. None of the reanalyses outperformed the others in all variables, at all altitudes and on both sides of the peninsula. Generally, NCEP‐CFSR and MERRA had the smallest errors in temperature profiles, JRA ‐55 had marginally the most accurate specific humidity profiles and NCEP‐CFSR had the best wind profiles. The reanalyses were coherent, although biased, on the western side of the A ntarctic P eninsula, but on the eastern side the spread was large. All the reanalyses underestimated the variability between the individual profiles of temperature and wind speed. The modern reanalyses with a sufficient spatial resolution and an adequate data assimilation method outperformed the others, especially on the eastern side.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here