Matches in SemOpenAlex for { <https://semopenalex.org/work/W2058904192> ?p ?o ?g. }
- W2058904192 abstract "In this study we investigate the radiative impact of ice supersaturated regions (ISSRs, i.e., cloud free air masses in the upper troposphere that are supersaturated with respect to ice) and thin cirrus. For this purpose we use corrected radiosonde data obtained from routine measurements over the meteorological observatory in Lindenberg, Germany. The radiative effect of the measured ice supersaturation is determined. By constructing an idealized profile from the measurement data the radiative properties of ISSRs and thin cirrus containing ice supersaturation were studied. The impact of ISSRs on the surface forcing is negligible but locally, within the vertical profile, changes in the heating rates up to 1 K d −1 for typical values of 130% relative humidity with respect to ice compared to the saturated profiles are found. This is also important for the local dynamics within the supersaturated layers. The outgoing longwave radiation due to the enhanced water vapor content inside ISSRs decreases up to 0.8 W m −2 . The radiative impact of thin cirrus is much stronger. Thin cirrus influence the surface budget, the top of the atmosphere radiation and the vertical profile of the heating rates. Changes in the outgoing longwave radiation and in the reflected shortwave flux at top of the atmosphere up to 64 W m −2 and 79 W m −2 , respectively, are possible. Changes in the surface flux (downward) up to 89 W m −2 are found. The maximal heating rate differences between thin cirrus and ISSR amount to 15 K d −1 . The radiative impact of thin cirrus clouds depends strongly on cloud ice content and the size of the ice crystals. Additionally, the radiative impact of cirrus formed by parameterizations not allowing ice supersaturations in large‐scale models is estimated. The errors due to artificially formed cirrus are quite large; differences up to 3 K d −1 in the vertical heating profiles and up to 38 and 40 W m −2 in the outgoing longwave radiation and the surface flux, respectively, are found. Thus we recommend using physically based parameterizations in GCMs which allow ice supersaturation." @default.
- W2058904192 created "2016-06-24" @default.
- W2058904192 creator A5041284859 @default.
- W2058904192 creator A5072453034 @default.
- W2058904192 creator A5091031341 @default.
- W2058904192 date "2007-12-15" @default.
- W2058904192 modified "2023-10-14" @default.
- W2058904192 title "Impact of ice supersaturated regions and thin cirrus on radiation in the midlatitudes" @default.
- W2058904192 cites W1587101236 @default.
- W2058904192 cites W1626331569 @default.
- W2058904192 cites W1756685254 @default.
- W2058904192 cites W1968405744 @default.
- W2058904192 cites W1974293595 @default.
- W2058904192 cites W1975249766 @default.
- W2058904192 cites W1975338397 @default.
- W2058904192 cites W1981445094 @default.
- W2058904192 cites W1981475041 @default.
- W2058904192 cites W1981992077 @default.
- W2058904192 cites W1982758878 @default.
- W2058904192 cites W1984537304 @default.
- W2058904192 cites W1990900389 @default.
- W2058904192 cites W1993621529 @default.
- W2058904192 cites W1997626366 @default.
- W2058904192 cites W2006841949 @default.
- W2058904192 cites W2008594745 @default.
- W2058904192 cites W2009503250 @default.
- W2058904192 cites W2016809654 @default.
- W2058904192 cites W2021257661 @default.
- W2058904192 cites W2038308040 @default.
- W2058904192 cites W2043072377 @default.
- W2058904192 cites W2045556497 @default.
- W2058904192 cites W2048819092 @default.
- W2058904192 cites W2052253420 @default.
- W2058904192 cites W2065209900 @default.
- W2058904192 cites W2071280329 @default.
- W2058904192 cites W2077913768 @default.
- W2058904192 cites W2080811170 @default.
- W2058904192 cites W2097750168 @default.
- W2058904192 cites W2108812349 @default.
- W2058904192 cites W2114042149 @default.
- W2058904192 cites W2115756842 @default.
- W2058904192 cites W2131765612 @default.
- W2058904192 cites W2135110893 @default.
- W2058904192 cites W2137223522 @default.
- W2058904192 cites W2137841131 @default.
- W2058904192 cites W2138970375 @default.
- W2058904192 cites W2140672778 @default.
- W2058904192 cites W2143346350 @default.
- W2058904192 cites W2145096958 @default.
- W2058904192 cites W2146948033 @default.
- W2058904192 cites W2160456125 @default.
- W2058904192 cites W2168032149 @default.
- W2058904192 cites W2170323839 @default.
- W2058904192 cites W2174648383 @default.
- W2058904192 cites W2176391878 @default.
- W2058904192 cites W2179705157 @default.
- W2058904192 cites W4234374142 @default.
- W2058904192 cites W4239615156 @default.
- W2058904192 doi "https://doi.org/10.1029/2007jd008449" @default.
- W2058904192 hasPublicationYear "2007" @default.
- W2058904192 type Work @default.
- W2058904192 sameAs 2058904192 @default.
- W2058904192 citedByCount "81" @default.
- W2058904192 countsByYear W20589041922012 @default.
- W2058904192 countsByYear W20589041922013 @default.
- W2058904192 countsByYear W20589041922014 @default.
- W2058904192 countsByYear W20589041922015 @default.
- W2058904192 countsByYear W20589041922016 @default.
- W2058904192 countsByYear W20589041922017 @default.
- W2058904192 countsByYear W20589041922018 @default.
- W2058904192 countsByYear W20589041922019 @default.
- W2058904192 countsByYear W20589041922020 @default.
- W2058904192 countsByYear W20589041922021 @default.
- W2058904192 countsByYear W20589041922022 @default.
- W2058904192 countsByYear W20589041922023 @default.
- W2058904192 crossrefType "journal-article" @default.
- W2058904192 hasAuthorship W2058904192A5041284859 @default.
- W2058904192 hasAuthorship W2058904192A5072453034 @default.
- W2058904192 hasAuthorship W2058904192A5091031341 @default.
- W2058904192 hasConcept C10899652 @default.
- W2058904192 hasConcept C120665830 @default.
- W2058904192 hasConcept C121332964 @default.
- W2058904192 hasConcept C125388846 @default.
- W2058904192 hasConcept C127313418 @default.
- W2058904192 hasConcept C147534773 @default.
- W2058904192 hasConcept C153294291 @default.
- W2058904192 hasConcept C153385146 @default.
- W2058904192 hasConcept C19369268 @default.
- W2058904192 hasConcept C200447597 @default.
- W2058904192 hasConcept C2776120014 @default.
- W2058904192 hasConcept C2779155178 @default.
- W2058904192 hasConcept C2779345167 @default.
- W2058904192 hasConcept C2780723968 @default.
- W2058904192 hasConcept C2781448682 @default.
- W2058904192 hasConcept C39432304 @default.
- W2058904192 hasConcept C65440619 @default.
- W2058904192 hasConcept C74902906 @default.
- W2058904192 hasConcept C91586092 @default.
- W2058904192 hasConcept C97355855 @default.
- W2058904192 hasConcept C99578197 @default.