AB

Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

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


Zapytanie: INTERTROPICAL CONVERGENCE ZONE
Liczba odnalezionych rekordów: 2



Przejście do opcji zmiany formatu | Wyświetl/ukryj etykiety | Wyświetlenie wyników w wersji do druku | Pobranie pliku do edytora | Nowe wyszukiwanie
1/2
Nr opisu: 0^b998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM^a009996.700^b009899.000^c009999.000^d009899.000202220222022High-resolution insight into the Holocene environmental history of the Burullus Lagoon in norther00000426000000000609AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://www.cambridge.org/core/journals/quaternary-research/article/abs/highresolution-insight-into-the-holocene-environmental-history-of-the-burullus-lagoon-in-northern-nile-delta-egypt/B3B5C71601138100^a0033-5894^bQ^e1096-0287^fA^hABC^iX^jXY^kQ016946^a003^b003^c2021-12-01, 14:27^d2023-06-28, 10:07^e3319038812^f3124769232^aHigh-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, Egypt^aQuaternary Research^a2022^bVol. 107^dp. 87--103^a0033-5894^b1096-0287^a2021/2022^a10.1017/qua.2021.63^aNitychoruk, Jerzy^cy^aclimate change^aFINAL_PUBLISHED^bCC-BY-NC-ND^cAT_PUBLICATION^eOPEN_JOURNAL^aThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed since the Middle Holocene by the Sebennitic branch of the Nile and marine intrusions through the Bughaz inlet. A sediment core (BO-1) was collected at the northeastern shore of the lagoon and sampled at centennial scale resolution in order to reconstruct the development of the lagoon. The results show that an initial and limited lagoon had developed at the end of the Early Holocene, but after a dry period ca. 7.2 cal ka BP it has been progressively transformed into a marshy area, with occasional inflows of sea water. Lower water level and higher salinity of the Burullus Lagoon at 6.0-5.5 and 4.8-4.2 cal ka BP reflected droughts in the Nile catchment. Thereafter, the river reactivated in the Burullus Lagoon area, and since 2.8 cal ka BP was accompanied by occasional inflows of sea water. Since ca. 0.8 cal ka BP, increased fluvial activity occurred in this part of the Nile delta, which terminated after construction of the Aswan dams in the twentieth century.^aEastern Mediterranean^aIntertropical Convergence Zone^alagoon^aNile delta^asea-level change^aSebennitic branch.300IF^a996600^b998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM^a009996.700^b009899.000^c009999.000^d009899.000202220222022High-resolution insight into the Holocene environmental history of the Burullus Lagoon in norther00000426000000000609AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://www.cambridge.org/core/journals/quaternary-research/article/abs/highresolution-insight-into-the-holocene-environmental-history-of-the-burullus-lagoon-in-northern-nile-delta-egypt/B3B5C71601138100^a0033-5894^bQ^e1096-0287^fA^hABC^iX^jXY^kQ016946^a003^b003^c2021-12-01, 14:27^d2023-06-28, 10:07^e3319038812^f3124769232^aHigh-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, Egypt^aQuaternary Research^a2022^bVol. 107^dp. 87--103^a0033-5894^b1096-0287^a2021/2022^a10.1017/qua.2021.63^aNitychoruk, Jerzy^cy^aclimate change^aFINAL_PUBLISHED^bCC-BY-NC-ND^cAT_PUBLICATION^eOPEN_JOURNAL^aThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed since the Middle Holocene by the Sebennitic branch of the Nile and marine intrusions through the Bughaz inlet. A sediment core (BO-1) was collected at the northeastern shore of the lagoon and sampled at centennial scale resolution in order to reconstruct the development of the lagoon. The results show that an initial and limited lagoon had developed at the end of the Early Holocene, but after a dry period ca. 7.2 cal ka BP it has been progressively transformed into a marshy area, with occasional inflows of sea water. Lower water level and higher salinity of the Burullus Lagoon at 6.0-5.5 and 4.8-4.2 cal ka BP reflected droughts in the Nile catchment. Thereafter, the river reactivated in the Burullus Lagoon area, and since 2.8 cal ka BP was accompanied by occasional inflows of sea water. Since ca. 0.8 cal ka BP, increased fluvial activity occurred in this part of the Nile delta, which terminated after construction of the Aswan dams in the twentieth century.^aEastern Mediterranean^aIntertropical Convergence Zone^alagoon^aNile delta^asea-level change^aSebennitic branch
Autorzy: , , .
Tytuł pracy:
Tytuł pracy w innym języku: NitychorukChenSalemZalatoriginal-article996600009996.7000033-5894003High-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, EgyptQuaternary Research20220033-58942021/202210.1017/qua.2021.63Nitychoruk, Jerzyclimate changeFINAL_PUBLISHEDThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed since the Middle Holocene by the Sebennitic branch of the Nile and marine intrusions through the Bughaz inlet. A sediment core (BO-1) was collected at the northeastern shore of the lagoon and sampled at centennial scale resolution in order to reconstruct the development of the lagoon. The results show that an initial and limited lagoon had developed at the end of the Early Holocene, but after a dry period ca. 7.2 cal ka BP it has been progressively transformed into a marshy area, with occasional inflows of sea water. Lower water level and higher salinity of the Burullus Lagoon at 6.0-5.5 and 4.8-4.2 cal ka BP reflected droughts in the Nile catchment. Thereafter, the river reactivated in the Burullus Lagoon area, and since 2.8 cal ka BP was accompanied by occasional inflows of sea water. Since ca. 0.8 cal ka BP, increased fluvial activity occurred in this part of the Nile delta, which terminated after construction of the Aswan dams in the twentieth century.Eastern MediterraneanIntertropical Convergence ZonelagoonNile deltasea-level changeSebennitic branch : Jerzy Antoni : Zhongyuan : Alaa : Abdelfattah : Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.300IF : 998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM : 009899.000 : Q : 003 : Vol. 107 : 1096-0287 : CC-BY-NC-ND
Miejsce wydania: NitychorukChenSalemZalatoriginal-article996600009996.7000033-5894003High-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, EgyptQuaternary Research20220033-58942021/202210.1017/qua.2021.63Nitychoruk, Jerzyclimate changeFINAL_PUBLISHEDThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed
Wydawca: Jerzy AntoniZhongyuanAlaaAbdelfattahOryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.300IF998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM009899.000Q003Vol. 1071096-0287CC-BY-NC-ND
Rok wydania: 033009999.0002021-12-01, 14:27yAT_PUBLICATION
Strony: NitychorukChenSalemZalatoriginal-article996600009996.7000033-5894003High-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, EgyptQuaternary Research20220033-58942021/202210.1017/qua.2021.63Nitychoruk, Jerzyclimate changeFINAL_PUBLISHEDThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed since the Middle Holocene by the Sebennitic branch of the Nile and marine intrusions through the Bughaz inlet. A sediment core (BO-1) was collected at the northeastern shore of the lagoon and sampled at centennial scale resolution in order to reconstruct the development of the lagoon. The results show that an initial and limited lagoon had developed at the end of the Early Holocene, but after a dry period ca. 7.2 cal ka BP it has been progressively transformed into a marshy area, with occasional inflows of sea water. Lower water level and higher salinity, Jerzy Antoni, Zhongyuan, Alaa, Abdelfattah, Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.300IF, 998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM, 009899.000, Q, 003, Vol. 107, 1096-0287, CC-BY-NC-ND, 033, , , , 009999.000, 2021-12-01, 14:27, y, AT_PUBLICATION, WNET0201, , , , 009899.000202220222022High-resolution insight into the Holocene environmental history of the Burullus Lagoon in norther00000426000000000609AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://www.cambridge.org/core/journals/quaternary-research/article/abs/highresolution-insight-into-the-holocene-environmental-history-of-the-burullus-lagoon-in-northern-nile-delta-egypt/B3B5C71601138100, 2023-06-28, 10:07, p. 87--103
Charakterystyka formalna:
Słowa kluczowe ang.: ;
Streszczenie:

2/2
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