FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2096814380> ?p ?o ?g. }

• W2096814380 endingPage "3496" @default.
• W2096814380 startingPage "3483" @default.
• W2096814380 abstract "The global distribution of ozone during the October 31, 1978, to May 6, 1993, observing lifetime of the Nimbus 7 total ozone mapping spectrometer (TOMS) is described, with emphasis on the low ozone amounts observed during 1992 and 1993. Ozone amount time series are extended beyond May 6, 1993, to the end of July 1993 using preliminary Meteor 3 TOMS data. Time series for zonally averaged ozone amounts show that there has not been a significant shift in the seasonal patterns of ozone maxima and minima caused by the Mount Pinatubo eruption or by the onset of very low ozone values during 1992 and 1993. There has been a relatively slow, nearly linear decrease in the amount of ozone over the entire globe from 1979 to the end of 1991, with rates ranging from no change at the equator to a 4–6% decrease per decade at midlatitudes and a 10–12% decrease per decade at higher latitudes. After the eruption of Mount Pinatubo during June 1991, the ozone amount decreased in the equatorial latitudes (10°S to 10°N) for about 6 months (−10 Dobson units (DU) between 0° and 10°S and −3 DU between 0° and 10°N). During 1992 and continuing into 1993, the rate of ozone decrease deviated from the previously linear trend with the onset of changes that were large in comparison with the historical range of ozone values from 1979 to 1991. The first of the large decreases in ozone amount occurred earlier, in February 1990 to May 1990, at 50°–70°N. At high northern latitudes, the 1993 decreased ozone amounts were about 12.5% below the envelope of historical values; at midlatitudes they were about 7% lower; and at low latitudes they were about 4% lower. Area‐weighted averages in the northern and southern hemispheres show that most of the 1992–1993 ozone losses have occurred in the northern hemisphere. The 1993 global average (70°S to 70°N) ozone amount is 3% below the 1979 to 1991 minimum, 5% below the historical envelope in the northern hemisphere, and near the lower boundary of the historical envelope in the southern hemisphere. In the 70°–60°S latitude band, the ozone losses between 1979 and 1993 have reduced the annual minimum amount to values below those seen in the equatorial regions." @default.
• W2096814380 created "2016-06-24" @default.
• W2096814380 creator A5038711026 @default.
• W2096814380 creator A5068535826 @default.
• W2096814380 date "1994-02-20" @default.
• W2096814380 modified "2023-09-26" @default.
• W2096814380 title "Low ozone amounts during 1992–1993 from Nimbus 7 and Meteor 3 total ozone mapping spectrometers" @default.
• W2096814380 cites W1964625810 @default.
• W2096814380 cites W1978262564 @default.
• W2096814380 cites W1984527430 @default.
• W2096814380 cites W1984797322 @default.
• W2096814380 cites W1987754140 @default.
• W2096814380 cites W1988264585 @default.
• W2096814380 cites W1992223523 @default.
• W2096814380 cites W1992472652 @default.
• W2096814380 cites W1997672520 @default.
• W2096814380 cites W1999249193 @default.
• W2096814380 cites W2002152913 @default.
• W2096814380 cites W2010415172 @default.
• W2096814380 cites W2013453552 @default.
• W2096814380 cites W2018291017 @default.
• W2096814380 cites W2027072908 @default.
• W2096814380 cites W2031044804 @default.
• W2096814380 cites W2041280456 @default.
• W2096814380 cites W2043591064 @default.
• W2096814380 cites W2046561232 @default.
• W2096814380 cites W2053250079 @default.
• W2096814380 cites W2054819507 @default.
• W2096814380 cites W2055698954 @default.
• W2096814380 cites W2065222008 @default.
• W2096814380 cites W2069545368 @default.
• W2096814380 cites W2072013831 @default.
• W2096814380 cites W2080959052 @default.
• W2096814380 cites W2085424101 @default.
• W2096814380 cites W2103617093 @default.
• W2096814380 cites W2108943534 @default.
• W2096814380 cites W2114433277 @default.
• W2096814380 cites W2147768051 @default.
• W2096814380 cites W2160017670 @default.
• W2096814380 cites W2160478964 @default.
• W2096814380 doi "https://doi.org/10.1029/93jd02594" @default.
• W2096814380 hasPublicationYear "1994" @default.
• W2096814380 type Work @default.
• W2096814380 sameAs 2096814380 @default.
• W2096814380 citedByCount "76" @default.
• W2096814380 countsByYear W20968143802013 @default.
• W2096814380 countsByYear W20968143802014 @default.
• W2096814380 countsByYear W20968143802015 @default.
• W2096814380 countsByYear W20968143802022 @default.
• W2096814380 crossrefType "journal-article" @default.
• W2096814380 hasAuthorship W2096814380A5038711026 @default.
• W2096814380 hasAuthorship W2096814380A5068535826 @default.
• W2096814380 hasConcept C108619276 @default.
• W2096814380 hasConcept C115719804 @default.
• W2096814380 hasConcept C122523270 @default.
• W2096814380 hasConcept C127313418 @default.
• W2096814380 hasConcept C12980444 @default.
• W2096814380 hasConcept C13280743 @default.
• W2096814380 hasConcept C141810719 @default.
• W2096814380 hasConcept C153294291 @default.
• W2096814380 hasConcept C163861444 @default.
• W2096814380 hasConcept C18101618 @default.
• W2096814380 hasConcept C205649164 @default.
• W2096814380 hasConcept C2778105581 @default.
• W2096814380 hasConcept C39432304 @default.
• W2096814380 hasConcept C49204034 @default.
• W2096814380 hasConcept C508106653 @default.
• W2096814380 hasConcept C91586092 @default.
• W2096814380 hasConceptScore W2096814380C108619276 @default.
• W2096814380 hasConceptScore W2096814380C115719804 @default.
• W2096814380 hasConceptScore W2096814380C122523270 @default.
• W2096814380 hasConceptScore W2096814380C127313418 @default.
• W2096814380 hasConceptScore W2096814380C12980444 @default.
• W2096814380 hasConceptScore W2096814380C13280743 @default.
• W2096814380 hasConceptScore W2096814380C141810719 @default.
• W2096814380 hasConceptScore W2096814380C153294291 @default.
• W2096814380 hasConceptScore W2096814380C163861444 @default.
• W2096814380 hasConceptScore W2096814380C18101618 @default.
• W2096814380 hasConceptScore W2096814380C205649164 @default.
• W2096814380 hasConceptScore W2096814380C2778105581 @default.
• W2096814380 hasConceptScore W2096814380C39432304 @default.
• W2096814380 hasConceptScore W2096814380C49204034 @default.
• W2096814380 hasConceptScore W2096814380C508106653 @default.
• W2096814380 hasConceptScore W2096814380C91586092 @default.
• W2096814380 hasIssue "D2" @default.
• W2096814380 hasLocation W20968143801 @default.
• W2096814380 hasOpenAccess W2096814380 @default.
• W2096814380 hasPrimaryLocation W20968143801 @default.
• W2096814380 hasRelatedWork W1480225841 @default.
• W2096814380 hasRelatedWork W1974572928 @default.
• W2096814380 hasRelatedWork W1996500857 @default.
• W2096814380 hasRelatedWork W1998723051 @default.
• W2096814380 hasRelatedWork W2110375598 @default.
• W2096814380 hasRelatedWork W2156494129 @default.
• W2096814380 hasRelatedWork W2168841033 @default.
• W2096814380 hasRelatedWork W286319613 @default.
• W2096814380 hasRelatedWork W770217661 @default.
• W2096814380 hasRelatedWork W821273240 @default.

• next