FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2014230630> ?p ?o ?g. }

• W2014230630 endingPage "239" @default.
• W2014230630 startingPage "215" @default.
• W2014230630 abstract "Spatiotemporal patterns of recent (1979–2008) air temperature trends are evaluated using three reanalysis datasets and radiosonde data. Our analysis demonstrates large discrepancies between the reanalysis datasets, possibly due to differences in the data assimilation procedures as well as sparseness and inhomogeneity of high-latitude observations. We test the robustness of arctic tropospheric warming based on the ERA-40 dataset. ERA-40 Arctic atmosphere temperatures tend to be closer to the observed ones in terms of root mean square error compared to other reanalysis products used in the article. However, changes in the ERA-40 data assimilation procedure produce unphysical jumps in atmospheric temperatures, which may be the likely reason for the elevated tropospheric warming trend in 1979–2002. NCEP/NCAR Reanalysis data show that the near-surface upward temperature trend over the same period is greater than the tropospheric trend, which is consistent with direct radiosonde observations and inconsistent with ERA-40 results. A change of sign in the winter temperature trend from negative to positive in the late 1980s is documented in the upper troposphere/lower stratosphere with a maximum over the Canadian Arctic, based on radiosonde data. This change from cooling to warming tendency is associated with weakening of the stratospheric polar vortex and shift of its center toward the Siberian coast and possibly can be explained by the changes in the dynamics of the Arctic Oscillation. This temporal pattern is consistent with multi-decadal variations of key arctic climate parameters like, for example, surface air temperature and oceanic freshwater content. Elucidating the mechanisms behind these changes will be critical to understanding the complex nature of high-latitude variability and its impact on global climate change." @default.
• W2014230630 created "2016-06-24" @default.
• W2014230630 creator A5006086733 @default.
• W2014230630 creator A5013790069 @default.
• W2014230630 creator A5020545468 @default.
• W2014230630 creator A5038829153 @default.
• W2014230630 creator A5080416102 @default.
• W2014230630 date "2011-08-23" @default.
• W2014230630 modified "2023-09-27" @default.
• W2014230630 title "Vertical structure of recent arctic warming from observed data and reanalysis products" @default.
• W2014230630 cites W1619408076 @default.
• W2014230630 cites W1832333051 @default.
• W2014230630 cites W1973001486 @default.
• W2014230630 cites W1978117718 @default.
• W2014230630 cites W1979694584 @default.
• W2014230630 cites W1980111930 @default.
• W2014230630 cites W1980831510 @default.
• W2014230630 cites W1986675024 @default.
• W2014230630 cites W1987097354 @default.
• W2014230630 cites W1989668498 @default.
• W2014230630 cites W1992652001 @default.
• W2014230630 cites W1993750261 @default.
• W2014230630 cites W1998853057 @default.
• W2014230630 cites W1999759982 @default.
• W2014230630 cites W2005628656 @default.
• W2014230630 cites W2011114191 @default.
• W2014230630 cites W2020297738 @default.
• W2014230630 cites W2022490268 @default.
• W2014230630 cites W2026675755 @default.
• W2014230630 cites W2027281809 @default.
• W2014230630 cites W2027649198 @default.
• W2014230630 cites W2042748717 @default.
• W2014230630 cites W2048783018 @default.
• W2014230630 cites W2049359727 @default.
• W2014230630 cites W2050056828 @default.
• W2014230630 cites W2050769910 @default.
• W2014230630 cites W2051483577 @default.
• W2014230630 cites W2055755179 @default.
• W2014230630 cites W2059072711 @default.
• W2014230630 cites W2059735239 @default.
• W2014230630 cites W2061420403 @default.
• W2014230630 cites W2064203536 @default.
• W2014230630 cites W2072551571 @default.
• W2014230630 cites W2073513089 @default.
• W2014230630 cites W2082349783 @default.
• W2014230630 cites W2093397974 @default.
• W2014230630 cites W2093401535 @default.
• W2014230630 cites W2093632513 @default.
• W2014230630 cites W2094464420 @default.
• W2014230630 cites W2096830549 @default.
• W2014230630 cites W2097045884 @default.
• W2014230630 cites W2105103805 @default.
• W2014230630 cites W2108497056 @default.
• W2014230630 cites W2113144013 @default.
• W2014230630 cites W2114094776 @default.
• W2014230630 cites W2122809335 @default.
• W2014230630 cites W2139756961 @default.
• W2014230630 cites W2145717465 @default.
• W2014230630 cites W2146377630 @default.
• W2014230630 cites W2161094102 @default.
• W2014230630 cites W2170460401 @default.
• W2014230630 cites W2173251738 @default.
• W2014230630 cites W2174886891 @default.
• W2014230630 cites W2177578417 @default.
• W2014230630 cites W4233772956 @default.
• W2014230630 cites W4250163396 @default.
• W2014230630 doi "https://doi.org/10.1007/s10584-011-0192-8" @default.
• W2014230630 hasPublicationYear "2011" @default.
• W2014230630 type Work @default.
• W2014230630 sameAs 2014230630 @default.
• W2014230630 citedByCount "51" @default.
• W2014230630 countsByYear W20142306302012 @default.
• W2014230630 countsByYear W20142306302013 @default.
• W2014230630 countsByYear W20142306302014 @default.
• W2014230630 countsByYear W20142306302015 @default.
• W2014230630 countsByYear W20142306302016 @default.
• W2014230630 countsByYear W20142306302017 @default.
• W2014230630 countsByYear W20142306302018 @default.
• W2014230630 countsByYear W20142306302019 @default.
• W2014230630 countsByYear W20142306302020 @default.
• W2014230630 countsByYear W20142306302021 @default.
• W2014230630 countsByYear W20142306302022 @default.
• W2014230630 crossrefType "journal-article" @default.
• W2014230630 hasAuthorship W2014230630A5006086733 @default.
• W2014230630 hasAuthorship W2014230630A5013790069 @default.
• W2014230630 hasAuthorship W2014230630A5020545468 @default.
• W2014230630 hasAuthorship W2014230630A5038829153 @default.
• W2014230630 hasAuthorship W2014230630A5080416102 @default.
• W2014230630 hasBestOaLocation W20142306302 @default.
• W2014230630 hasConcept C111368507 @default.
• W2014230630 hasConcept C11999413 @default.
• W2014230630 hasConcept C125405218 @default.
• W2014230630 hasConcept C127313418 @default.
• W2014230630 hasConcept C132651083 @default.
• W2014230630 hasConcept C14932015 @default.
• W2014230630 hasConcept C153294291 @default.
• W2014230630 hasConcept C163861444 @default.
• W2014230630 hasConcept C205649164 @default.

• next