AB

Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

Baza tworzona przez Bibliotekę Akademii Bialskiej im. Jana Pawła II.


Zapytanie: PALAEOWESTERLIES
Liczba odnalezionych rekordów: 1



Przejście do opcji zmiany formatu | Wyświetl/ukryj etykiety | Wyświetlenie wyników w wersji do druku | Pobranie pliku do edytora | Nowe wyszukiwanie
1/1
Autorzy: , , , , Qianli Marcin Izabela Anna Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.833IF 998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM 009899.000 Q 003 Vol. 528 Narodowe Centrum Nauki SunSzymanekGałeckaTołoczko-Pasekoriginal-article996066009996.1670031-0182003Cyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records in the Faiyum Oasis, EgyptPalaeogeography, Palaeoclimatology, Palaeoecology20190031-01822019/202010.1016/j.palaeo.2019.04.032Nitychoruk, JerzyholoceneKopia dostępna w Sekcji Bibliometrii.Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego EgiptuDuring African Humid Period in the Holocene when the summer Intertropical Convergence Zone migrated to its northernmost position, the Qarun Lake in the Faiyum Oasis in Egypt was fed with regular inflows from the Nile River and rainfall brought by the Mediterranean winter circulation. Finely-laminated lake sediments, dated at 8.5-6.7 cal kyr B.P., were examined in terms of lithology, geochemistry, microfossils (diatom, pollen) and magnetic susceptibility. Based on the inferred geographical derivation of pollen, the environmental affiliation of diatom taxa and geochemistry of lake sediments, wind trajectories were distinguished, related to two main atmospheric circulation phases. During the earlier phase (8.50-7.83 cal kyr B.P.) there were northwestern wind trajectories followed by southern ones and during the later phase (7.83-6.70 cal kyr B.P.), the northern winds were followed by northwestern and southern ones. Northwestern and northern winds brought winter rainfall and caused water turbulence in the lake, and the southern winds were associated with regional aridification. This scenario of atmospheric circulation in northeastern Africa extends significantly our understanding of key modes of climatic variability and wind trajectories in the Early to Middle Holocene (Greenlandian to Northgrippian) transition.atmospheric circulationIntertropical Convergence Zonepalaeowesterliespollen recorddiatoms.
Szczegóły:
Oznaczenie wydania: SunSzymanekGałecka
Miejsce wydania: SunSzymanekGałeckaTołoczko-Pasekoriginal-article996066009996.1670031-0182003Cyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records in the Faiyum Oasis, EgyptPalaeogeography, Palaeoclimatology, Palaeoecology20190031-01822019/202010.1016/j.palaeo.2019.04.032Nitychoruk, JerzyholoceneKopia dostępna w Sekcji Bibliometrii.Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego EgiptuDuring African Humid Period in the Holocene when the summer Intertropical Convergence Zone migrated to its northernmost position, the Qarun Lake in the Faiyum Oasis in Egypt was fed with regular inflows from the Nile River and rainfall brought by the Mediterranean winter circulation. Finely-laminated lake sediments, dated at 8.5-6.7 cal kyr B.P., were examined in terms of lithology, geochemistry, microfossils (diatom, pollen) and magnetic susceptibility. Based on the inferred geographical derivation of pollen, the environmental affiliation of diatom taxa and geochemistry of lake sediments, wind trajectories were distinguished, related to two main atmospheric circulation phases. During the earlier phase (8.50-7.83 cal kyr B.P.) there were northwestern wind trajectories followed by southern ones and during the later phase (7.83-6.70 cal kyr B.P.), the northern winds were followed by northwestern and southern ones. Northwestern and northern winds brought winter rainfall and caused water turbulence in the lake, and the southern winds were associated with regional aridification. This scenario of atmospheric circulation in northeastern Africa extends significantly our understanding of key modes of climatic variability and wind trajectories in the Early to Middle Holocene (Greenlandian to Northgrippian) transition.atmospheric circulationIntertropical Convergence Zonepalaeowesterliespollen recorddiatoms
Wydawca: AalaQianliMarcinIzabelaAnnaOryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.833IF998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM009899.000Q003Vol. 528Narodowe Centrum Nauki
Rok wydania: 009999.0002019-11-07, 09:20yDEC-2012/05/B/ST10/00558
Charakterystyka wg MNiSW:
Język publikacji: ACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM^a009996.167^b009899.000^c009999.000^d009899.000201920192019Cyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records i00000381710000001226AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGPRACA RECENZOWANA100^a0031-0182^bQ^iX^jXY^kQ015676^a003^b003^c2019-11-07, 09:20^d2020-06-30, 11:30^e3519979319^f3424749109^aCyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records in the Faiyum Oasis, Egypt^aPalaeogeography, Palaeoclimatology, Palaeoecology^a2019^bVol. 528^dp. 120--132^a0031-0182^a2019/2020^a10.1016/j.palaeo.2019.04.032^aNitychoruk, Jerzy^cy^aholocene^aKopia dostępna w Sekcji Bibliometrii.^aRekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego Egiptu^bNarodowe Centrum Nauki^cDEC-2012/05/B/ST10/00558^aDuring African Humid Period in the Holocene when the summer Intertropical Convergence Zone migrated to its northernmost position, the Qarun Lake in the Faiyum Oasis in Egypt was fed with regular inflows from the Nile River and rainfall brought by the Mediterranean winter circulation. Finely-laminated lake sediments, dated at 8.5-6.7 cal kyr B.P., were examined in terms of lithology, geochemistry, microfossils (diatom, pollen) and magnetic susceptibility. Based on the inferred geographical derivation of pollen, the environmental affiliation of diatom taxa and geochemistry of lake sediments, wind trajectories were distinguished, related to two main atmospheric circulation phases. During the earlier phase (8.50-7.83 cal kyr B.P.) there were northwestern wind trajectories followed by southern ones and during the later phase (7.83-6.70 cal kyr B.P.), the northern winds were followed by northwestern and southern ones. Northwestern and northern winds brought winter rainfall and caused water turbulence in the lake, and the southern winds were associated with regional aridification. This scenario of atmospheric circulation in northeastern Africa extends significantly our understanding of key modes of climatic variability and wind trajectories in the Early to Middle Holocene (Greenlandian to Northgrippian) transition.^aatmospheric circulation^aIntertropical Convergence Zone^apalaeowesterlies^apollen record^adiatoms
Wskaźnik Impact Factor ISI: ACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM^a009996.167^b009899.000^c009999.000^d009899.000201920192019Cyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records i00000381710000001226AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGPRACA RECENZOWANA100^a0031-0182^bQ^iX^jXY^kQ015676^a003^b003^c2019-11-07, 09:20^d2020-06-30, 11:30^e3519979319^f3424749109^aCyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records in the Faiyum Oasis, Egypt^aPalaeogeography, Palaeoclimatology, Palaeoecology^a2019^bVol. 528^dp. 120--132^a0031-0182^a2019/2020^a10.1016/j.palaeo.2019.04.032^aNitychoruk, Jerzy^cy^aholocene^aKopia dostępna w Sekcji Bibliometrii.^aRekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego Egiptu^bNarodowe Centrum Nauki^cDEC-2012/05/B/ST10/00558^aDuring African Humid Period in the Holocene when the summer Intertropical Convergence Zone migrated to its northernmost position, the Qarun Lake in the Faiyum Oasis in Egypt was fed with regular inflows from the Nile River and rainfall brought by the Mediterranean winter circulation. Finely-laminated lake sediments, dated at 8.5-6.7 cal kyr B.P., were examined in terms of lithology, geochemistry, microfossils (diatom, pollen) and magnetic susceptibility. Based on the inferred geographical derivation of pollen, the environmental affiliation of diatom taxa and geochemistry of lake sediments, wind trajectories were distinguished, related to two main atmospheric circulation phases. During the earlier phase (8.50-7.83 cal kyr B.P.) there were northwestern wind trajectories followed by southern ones and during the later phase (7.83-6.70 cal kyr B.P.), the northern winds were followed by northwestern and southern ones. Northwestern and northern winds brought winter rainfall and caused water turbulence in the lake, and the southern winds were associated with regional aridification. This scenario of atmospheric circulation in northeastern Africa extends significantly our understanding of key modes of climatic variability and wind trajectories in the Early to Middle Holocene (Greenlandian to Northgrippian) transition.^aatmospheric circulation^aIntertropical Convergence Zone^apalaeowesterlies^apollen record^adiatoms
Praca recenzowana
Słowa kluczowe ang.: pSalem Aala^rSalem^sAala^u^t^qSalem A^w^x0000028618^zSalem Aala^aSun
Słowa kluczowe ang.: ;
Uwaga:
Inne bazy podające opis:


  • DOI:

      Wyświetl ponownie stosując format:
    • Wyświetl/ukryj etykiety | Wyświetlenie wyników w wersji do druku | Pobranie pliku do edytora | Nowe wyszukiwanie | Biblioteka AB