FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2111695227> ?p ?o ?g. }

• W2111695227 endingPage "2154" @default.
• W2111695227 startingPage "2131" @default.
• W2111695227 abstract "Abstract. The aim of this study is to theoretically investigate the sensitivity of the Multi-angle Imaging SpectroRadiometer (MISR) operational (version 22) Dark Water retrieval algorithm to aerosol non-sphericity over the global oceans under actual observing conditions, accounting for current algorithm assumptions. Non-spherical (dust) aerosol models, which were introduced in version 16 of the MISR aerosol product, improved the quality and coverage of retrievals in dusty regions. Due to the sensitivity of the retrieval to the presence of non-spherical aerosols, the MISR aerosol product has been successfully used to track the location and evolution of mineral dust plumes from the Sahara across the Atlantic, for example. However, the MISR global non-spherical aerosol optical depth (AOD) fraction product has been found to have several climatological artifacts superimposed on valid detections of mineral dust, including high non-spherical fraction in the Southern Ocean and seasonally variable bands of high non-sphericity. In this paper we introduce a formal approach to examine the ability of the operational MISR Dark Water algorithm to distinguish among various spherical and non-spherical particles as a function of the variable MISR viewing geometry. We demonstrate the following under the criteria currently implemented: (1) Dark Water retrieval sensitivity to particle non-sphericity decreases for AOD below about 0.1 primarily due to an unnecessarily large lower bound imposed on the uncertainty in MISR observations at low light levels, and improves when this lower bound is removed; (2) Dark Water retrievals are able to distinguish between the spherical and non-spherical particles currently used for all MISR viewing geometries when the AOD exceeds 0.1; (3) the sensitivity of the MISR retrievals to aerosol non-sphericity varies in a complex way that depends on the sampling of the scattering phase function and the contribution from multiple scattering; and (4) non-sphericity artifacts occur at those view-illumination geometries where dust aerosols are indistinguishable from certain types of cirrus particles. Based on these results, we suggest that interested parties use caution with the version 22 MISR Dark Water aerosol non-sphericity product in situations where cirrus may be present." @default.
• W2111695227 created "2016-06-24" @default.
• W2111695227 creator A5013757592 @default.
• W2111695227 creator A5059352820 @default.
• W2111695227 creator A5061193396 @default.
• W2111695227 creator A5085702823 @default.
• W2111695227 date "2013-08-27" @default.
• W2111695227 modified "2023-09-30" @default.
• W2111695227 title "MISR Dark Water aerosol retrievals: operational algorithm sensitivity to particle non-sphericity" @default.
• W2111695227 cites W1940907344 @default.
• W2111695227 cites W1967432488 @default.
• W2111695227 cites W1968443022 @default.
• W2111695227 cites W1969360670 @default.
• W2111695227 cites W1982339703 @default.
• W2111695227 cites W1982613823 @default.
• W2111695227 cites W1985090550 @default.
• W2111695227 cites W1985998218 @default.
• W2111695227 cites W1989890939 @default.
• W2111695227 cites W1991096607 @default.
• W2111695227 cites W1992317562 @default.
• W2111695227 cites W1997071220 @default.
• W2111695227 cites W2009612094 @default.
• W2111695227 cites W2018024014 @default.
• W2111695227 cites W2020043171 @default.
• W2111695227 cites W2020432593 @default.
• W2111695227 cites W2024891763 @default.
• W2111695227 cites W2025174696 @default.
• W2111695227 cites W2029882954 @default.
• W2111695227 cites W2033156080 @default.
• W2111695227 cites W2034000133 @default.
• W2111695227 cites W2034158030 @default.
• W2111695227 cites W2040869203 @default.
• W2111695227 cites W2041928928 @default.
• W2111695227 cites W2044641411 @default.
• W2111695227 cites W2044940833 @default.
• W2111695227 cites W2045150402 @default.
• W2111695227 cites W2046198712 @default.
• W2111695227 cites W2048512417 @default.
• W2111695227 cites W2054279173 @default.
• W2111695227 cites W2061716049 @default.
• W2111695227 cites W2071738444 @default.
• W2111695227 cites W2072430404 @default.
• W2111695227 cites W2078932557 @default.
• W2111695227 cites W2082000275 @default.
• W2111695227 cites W2085438990 @default.
• W2111695227 cites W2086463688 @default.
• W2111695227 cites W2087651237 @default.
• W2111695227 cites W2089891032 @default.
• W2111695227 cites W2090989407 @default.
• W2111695227 cites W2091258005 @default.
• W2111695227 cites W2092889986 @default.
• W2111695227 cites W2094216302 @default.
• W2111695227 cites W2098065523 @default.
• W2111695227 cites W2098344723 @default.
• W2111695227 cites W2100228139 @default.
• W2111695227 cites W2102553184 @default.
• W2111695227 cites W2102834380 @default.
• W2111695227 cites W2110890760 @default.
• W2111695227 cites W2111111029 @default.
• W2111695227 cites W2116035652 @default.
• W2111695227 cites W2118339035 @default.
• W2111695227 cites W2120397945 @default.
• W2111695227 cites W2122943628 @default.
• W2111695227 cites W2125855972 @default.
• W2111695227 cites W2129479849 @default.
• W2111695227 cites W2132134745 @default.
• W2111695227 cites W2135260575 @default.
• W2111695227 cites W2139937607 @default.
• W2111695227 cites W2142529295 @default.
• W2111695227 cites W2146737207 @default.
• W2111695227 cites W2146833894 @default.
• W2111695227 cites W2154889667 @default.
• W2111695227 cites W2159481845 @default.
• W2111695227 cites W2162246342 @default.
• W2111695227 cites W2165696931 @default.
• W2111695227 cites W2167604263 @default.
• W2111695227 cites W2167672969 @default.
• W2111695227 cites W2168466445 @default.
• W2111695227 cites W2171687450 @default.
• W2111695227 cites W2179103847 @default.
• W2111695227 cites W2204838419 @default.
• W2111695227 doi "https://doi.org/10.5194/amt-6-2131-2013" @default.
• W2111695227 hasPublicationYear "2013" @default.
• W2111695227 type Work @default.
• W2111695227 sameAs 2111695227 @default.
• W2111695227 citedByCount "35" @default.
• W2111695227 countsByYear W21116952272014 @default.
• W2111695227 countsByYear W21116952272015 @default.
• W2111695227 countsByYear W21116952272016 @default.
• W2111695227 countsByYear W21116952272017 @default.
• W2111695227 countsByYear W21116952272018 @default.
• W2111695227 countsByYear W21116952272019 @default.
• W2111695227 countsByYear W21116952272020 @default.
• W2111695227 countsByYear W21116952272021 @default.
• W2111695227 countsByYear W21116952272022 @default.
• W2111695227 countsByYear W21116952272023 @default.
• W2111695227 crossrefType "journal-article" @default.
• W2111695227 hasAuthorship W2111695227A5013757592 @default.

• next