FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2130625229> ?p ?o ?g. }

• W2130625229 endingPage "3526" @default.
• W2130625229 startingPage "3506" @default.
• W2130625229 abstract "Abstract The direct radiative effect of aerosols (DREA) is defined as the difference between radiative fluxes in the absence and presence of aerosols. In this study, the direct radiative effect of aerosols is estimated for 46 months (March 2000–December 2003) of merged Clouds and the Earth’s Radiant Energy System (CERES) and Moderate Resolution Imaging Spectroradiometer (MODIS) Terra global measurements over ocean. This analysis includes the contribution from clear regions in both clear and partly cloudy CERES footprints. MODIS–CERES narrow-to-broadband regressions are developed to convert clear-sky MODIS narrowband radiances to broadband shortwave (SW) radiances, and CERES clear-sky angular distribution models (ADMs) are used to estimate the corresponding top-of-atmosphere (TOA) radiative fluxes that are needed to determine the DREA. Clear-sky MODIS pixels are identified using two independent cloud masks: (i) the NOAA/National Environmental Satellite, Data, and Information Service (NESDIS) algorithm that is used for inferring aerosol properties from MODIS on the CERES Single Scanner Footprint TOA/Surface Fluxes and Clouds (SSF) product (NOAA SSF); and (ii) the standard algorithm that is used by the MODIS aerosol group to produce the MODIS aerosol product (MOD04). Over global oceans, direct radiative cooling by aerosols for clear scenes that are identified from MOD04 is estimated to be 40% larger than for clear scenes from NOAA SSF (5.5 compared to 3.8 W m−2). Regionally, differences are largest in areas that are affected by dust aerosol, such as oceanic regions that are adjacent to the Sahara and Saudi Arabian deserts, and in northern Pacific Ocean regions that are influenced by dust transported from Asia. The net total-sky (clear and cloudy) DREA is negative (cooling) and is estimated to be −2.0 W m−2 from MOD04, and −1.6 W m−2 from NOAA SSF. The DREA is shown to have pronounced seasonal cycles in the Northern Hemisphere and large year-to-year fluctuations near deserts. However, no systematic trend in deseasonalized anomalies of the DREA is observed over the 46-month time series that is considered." @default.
• W2130625229 created "2016-06-24" @default.
• W2130625229 creator A5061801950 @default.
• W2130625229 creator A5088530785 @default.
• W2130625229 date "2005-09-01" @default.
• W2130625229 modified "2023-10-10" @default.
• W2130625229 title "Top-of-Atmosphere Direct Radiative Effect of Aerosols over Global Oceans from Merged CERES and MODIS Observations" @default.
• W2130625229 cites W1963824509 @default.
• W2130625229 cites W1968104874 @default.
• W2130625229 cites W1969583657 @default.
• W2130625229 cites W1973264299 @default.
• W2130625229 cites W1975811916 @default.
• W2130625229 cites W1977490942 @default.
• W2130625229 cites W1979058762 @default.
• W2130625229 cites W1985573540 @default.
• W2130625229 cites W1989790045 @default.
• W2130625229 cites W2011709773 @default.
• W2130625229 cites W2013689051 @default.
• W2130625229 cites W2015309381 @default.
• W2130625229 cites W2023456331 @default.
• W2130625229 cites W2025809975 @default.
• W2130625229 cites W2030038151 @default.
• W2130625229 cites W2038712866 @default.
• W2130625229 cites W2045465689 @default.
• W2130625229 cites W2050848450 @default.
• W2130625229 cites W2057262021 @default.
• W2130625229 cites W2117640593 @default.
• W2130625229 cites W2131041319 @default.
• W2130625229 cites W2135818207 @default.
• W2130625229 cites W2137094214 @default.
• W2130625229 cites W2138977661 @default.
• W2130625229 cites W2141433795 @default.
• W2130625229 cites W2145265567 @default.
• W2130625229 cites W2148186985 @default.
• W2130625229 cites W2158478006 @default.
• W2130625229 cites W2172603579 @default.
• W2130625229 cites W2176014542 @default.
• W2130625229 cites W2176809068 @default.
• W2130625229 cites W2179235199 @default.
• W2130625229 cites W2180346849 @default.
• W2130625229 cites W4254887142 @default.
• W2130625229 doi "https://doi.org/10.1175/jcli3504.1" @default.
• W2130625229 hasPublicationYear "2005" @default.
• W2130625229 type Work @default.
• W2130625229 sameAs 2130625229 @default.
• W2130625229 citedByCount "166" @default.
• W2130625229 countsByYear W21306252292012 @default.
• W2130625229 countsByYear W21306252292013 @default.
• W2130625229 countsByYear W21306252292014 @default.
• W2130625229 countsByYear W21306252292015 @default.
• W2130625229 countsByYear W21306252292016 @default.
• W2130625229 countsByYear W21306252292017 @default.
• W2130625229 countsByYear W21306252292018 @default.
• W2130625229 countsByYear W21306252292019 @default.
• W2130625229 countsByYear W21306252292020 @default.
• W2130625229 countsByYear W21306252292021 @default.
• W2130625229 countsByYear W21306252292022 @default.
• W2130625229 crossrefType "journal-article" @default.
• W2130625229 hasAuthorship W2130625229A5061801950 @default.
• W2130625229 hasAuthorship W2130625229A5088530785 @default.
• W2130625229 hasBestOaLocation W21306252291 @default.
• W2130625229 hasConcept C121332964 @default.
• W2130625229 hasConcept C127313418 @default.
• W2130625229 hasConcept C1276947 @default.
• W2130625229 hasConcept C153294291 @default.
• W2130625229 hasConcept C19269812 @default.
• W2130625229 hasConcept C199390426 @default.
• W2130625229 hasConcept C205649164 @default.
• W2130625229 hasConcept C23690007 @default.
• W2130625229 hasConcept C2776272892 @default.
• W2130625229 hasConcept C2777007095 @default.
• W2130625229 hasConcept C2777634575 @default.
• W2130625229 hasConcept C2779345167 @default.
• W2130625229 hasConcept C39432304 @default.
• W2130625229 hasConcept C62520636 @default.
• W2130625229 hasConcept C62649853 @default.
• W2130625229 hasConcept C65440619 @default.
• W2130625229 hasConcept C68130645 @default.
• W2130625229 hasConcept C73329638 @default.
• W2130625229 hasConcept C74902906 @default.
• W2130625229 hasConcept C91586092 @default.
• W2130625229 hasConceptScore W2130625229C121332964 @default.
• W2130625229 hasConceptScore W2130625229C127313418 @default.
• W2130625229 hasConceptScore W2130625229C1276947 @default.
• W2130625229 hasConceptScore W2130625229C153294291 @default.
• W2130625229 hasConceptScore W2130625229C19269812 @default.
• W2130625229 hasConceptScore W2130625229C199390426 @default.
• W2130625229 hasConceptScore W2130625229C205649164 @default.
• W2130625229 hasConceptScore W2130625229C23690007 @default.
• W2130625229 hasConceptScore W2130625229C2776272892 @default.
• W2130625229 hasConceptScore W2130625229C2777007095 @default.
• W2130625229 hasConceptScore W2130625229C2777634575 @default.
• W2130625229 hasConceptScore W2130625229C2779345167 @default.
• W2130625229 hasConceptScore W2130625229C39432304 @default.
• W2130625229 hasConceptScore W2130625229C62520636 @default.
• W2130625229 hasConceptScore W2130625229C62649853 @default.
• W2130625229 hasConceptScore W2130625229C65440619 @default.
• W2130625229 hasConceptScore W2130625229C68130645 @default.

• next