FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1995346522> ?p ?o ?g. }

• W1995346522 endingPage "31125" @default.
• W1995346522 startingPage "31109" @default.
• W1995346522 abstract "Diurnal and semidiurnal variations in surface winds and wind divergence over the globe (50°S-70°N) are documented using 3-hourly wind observations from ∼10,000 land stations and available marine reports during 1976–1997. A strong diurnal cycle in surface winds is found over land areas (strongest over high terrain and in summer) with an amplitude of 0.6–1.1 m/s for wind speed and 0.5–0.7 m/s for the zonal and meridional wind components. Surface wind speed peaks in the early afternoon over most of the globe. It is suggested that increased downward turbulent mixing of momentum during the day could be one of the main causes for the early afternoon maximum of surface wind speed. The diurnal anomalies of surface wind divergence tend to be out of phase in adjacent regions. In particular, land areas (except for extreme inland locations) exhibit maximum divergence around dawn (0600–0800 local solar time (LST)), while nearby oceanic regions have their maximum divergence in the evening (1700–1900 LST). Thus, there is evidence for a large-scale diurnal circulation in which surface air rises and converges over the continents and sinks and diverges over nearby oceans in the afternoon and early evening, and the opposite occurs in the early morning. Over the tropical Atlantic and Pacific Oceans (10°S-10°N), a zonally coherent pattern of maximum convergence (divergence) north (south) of the equator around 0900–1200 LST is generally similar to the latitudinal profile of the mean daily divergence, indicative of an enhancement of the local Hadley cell around 1030 LST relative to the daily mean. Another zonally coherent north-south dipole occurs over the North Pacific, with maximum surface wind divergence (convergence) around 0600–0800 LST in the subtropics (midlatitudes). This phase pattern correlates with cloud cover over the two regions. Over the United States, surface divergence peaks around 0600 LST in the west and the east and around 2000 LST in the center." @default.
• W1995346522 created "2016-06-24" @default.
• W1995346522 creator A5069099218 @default.
• W1995346522 creator A5083255781 @default.
• W1995346522 date "1999-12-01" @default.
• W1995346522 modified "2023-10-03" @default.
• W1995346522 title "Diurnal and semidiurnal variations in global surface wind and divergence fields" @default.
• W1995346522 cites W1883859813 @default.
• W1995346522 cites W1974992710 @default.
• W1995346522 cites W1976345358 @default.
• W1995346522 cites W1978685552 @default.
• W1995346522 cites W1979256008 @default.
• W1995346522 cites W1979945830 @default.
• W1995346522 cites W1988134363 @default.
• W1995346522 cites W1990402820 @default.
• W1995346522 cites W1993919755 @default.
• W1995346522 cites W1994927247 @default.
• W1995346522 cites W1995922295 @default.
• W1995346522 cites W2000058221 @default.
• W1995346522 cites W2016582563 @default.
• W1995346522 cites W2039534721 @default.
• W1995346522 cites W2041861589 @default.
• W1995346522 cites W2043621832 @default.
• W1995346522 cites W2050651661 @default.
• W1995346522 cites W2052704844 @default.
• W1995346522 cites W2054112955 @default.
• W1995346522 cites W2056286716 @default.
• W1995346522 cites W2056607997 @default.
• W1995346522 cites W2058472632 @default.
• W1995346522 cites W2072886461 @default.
• W1995346522 cites W2080658792 @default.
• W1995346522 cites W2082600560 @default.
• W1995346522 cites W2082684467 @default.
• W1995346522 cites W2093281313 @default.
• W1995346522 cites W2093839132 @default.
• W1995346522 cites W2100262392 @default.
• W1995346522 cites W2160818201 @default.
• W1995346522 cites W2162277775 @default.
• W1995346522 cites W2173631438 @default.
• W1995346522 cites W2173962251 @default.
• W1995346522 cites W2176353678 @default.
• W1995346522 cites W2279239392 @default.
• W1995346522 cites W2605581224 @default.
• W1995346522 doi "https://doi.org/10.1029/1999jd900927" @default.
• W1995346522 hasPublicationYear "1999" @default.
• W1995346522 type Work @default.
• W1995346522 sameAs 1995346522 @default.
• W1995346522 citedByCount "191" @default.
• W1995346522 countsByYear W19953465222012 @default.
• W1995346522 countsByYear W19953465222013 @default.
• W1995346522 countsByYear W19953465222014 @default.
• W1995346522 countsByYear W19953465222015 @default.
• W1995346522 countsByYear W19953465222016 @default.
• W1995346522 countsByYear W19953465222017 @default.
• W1995346522 countsByYear W19953465222018 @default.
• W1995346522 countsByYear W19953465222019 @default.
• W1995346522 countsByYear W19953465222020 @default.
• W1995346522 countsByYear W19953465222021 @default.
• W1995346522 countsByYear W19953465222022 @default.
• W1995346522 countsByYear W19953465222023 @default.
• W1995346522 crossrefType "journal-article" @default.
• W1995346522 hasAuthorship W1995346522A5069099218 @default.
• W1995346522 hasAuthorship W1995346522A5083255781 @default.
• W1995346522 hasConcept C121332964 @default.
• W1995346522 hasConcept C127313418 @default.
• W1995346522 hasConcept C138885662 @default.
• W1995346522 hasConcept C153294291 @default.
• W1995346522 hasConcept C207390915 @default.
• W1995346522 hasConcept C41895202 @default.
• W1995346522 hasConcept C49204034 @default.
• W1995346522 hasConcept C8058405 @default.
• W1995346522 hasConcept C91586092 @default.
• W1995346522 hasConceptScore W1995346522C121332964 @default.
• W1995346522 hasConceptScore W1995346522C127313418 @default.
• W1995346522 hasConceptScore W1995346522C138885662 @default.
• W1995346522 hasConceptScore W1995346522C153294291 @default.
• W1995346522 hasConceptScore W1995346522C207390915 @default.
• W1995346522 hasConceptScore W1995346522C41895202 @default.
• W1995346522 hasConceptScore W1995346522C49204034 @default.
• W1995346522 hasConceptScore W1995346522C8058405 @default.
• W1995346522 hasConceptScore W1995346522C91586092 @default.
• W1995346522 hasIssue "D24" @default.
• W1995346522 hasLocation W19953465221 @default.
• W1995346522 hasOpenAccess W1995346522 @default.
• W1995346522 hasPrimaryLocation W19953465221 @default.
• W1995346522 hasRelatedWork W1998520275 @default.
• W1995346522 hasRelatedWork W2021653241 @default.
• W1995346522 hasRelatedWork W2129232412 @default.
• W1995346522 hasRelatedWork W2130125019 @default.
• W1995346522 hasRelatedWork W2953907617 @default.
• W1995346522 hasRelatedWork W2977349066 @default.
• W1995346522 hasRelatedWork W2990817032 @default.
• W1995346522 hasRelatedWork W2995980713 @default.
• W1995346522 hasRelatedWork W3023536432 @default.
• W1995346522 hasRelatedWork W4224436598 @default.
• W1995346522 hasVolume "104" @default.
• W1995346522 isParatext "false" @default.
• W1995346522 isRetracted "false" @default.

• next