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Zapytanie: ATMOSPHERIC CIRCULATION
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Nr opisu: 0000000468AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttp://www.jeeng.net/The-Meteorological-Conditions-of-Precipitation-Deficits-in-the-Cultivation-of-Winter,168349,0,2.html100^bQ^e2299-8993^iX^jXY^kQ010838^a003^b003^c2023-08-16, 10:09^d2023-09-18, 12:23^e3122889230^f3121869016^aThe Meteorological Conditions of Precipitation Deficits in the Cultivation of Winter Wheat in Central and Eastern Poland^aJournal of Ecological Engineering^a2023^bVol. 24^cissue 9^dp. 50--62^a2299-8993^b2081-139X^a2022/2023^a10.12911/22998993/168349^aBaranowska, Alicja^cx^aair temperature^aWpływ czynników środowiskowych i agrotechnicznych na cechy jakościowe i plonowanie wybranych gatunków roślin^bFundusz Rozwoju Nauki PSW^cPB/26/2020^aFINAL_PUBLISHED^bCC-BY^cAT_PUBLICATION^eOPEN_JOURNAL^aThe problem of precipitation deficits constitutes an issue that is significant on a global, re-gional, and local scale, particularly in the aspect of climate warming. The purpose of this research was to determine the amount, frequency and trends of precipitation deficits in the cultivation of winter wheat in central and eastern Poland, over a period of fifty years (from 1971 to 2020). This study used the values of average monthly air temperatures, as well as monthly total precipitation, decadal precipitation needs of winter wheat within central and eastern Poland. Based on the performed research, both spatial and temporal differences were observed in the scope of the amount and frequency of precipitation deficits in the cultivation of winter wheat. The lowest risk of precipitation deficits was found in May (from 15% to 32%), which is a critical month in the cultivation of this plant in Poland, while the highest risk of precipitation deficits was observed in June (from 22% to 56%), which is an unfavourable phenomenon, because winter wheat is in the so-called grain filling phase since mid-June. It was also found that there is a statistically significant upward trend of the winter wheat's precipitation needs in April, June, and July. An increase in the inflow of warm and dry air masses from the southern sectors was one of the factors impacting the amount and frequency of precipitation deficits in the cultivation of wheat. The problem of climate warming that has been increasing in recent years, and - as a consequence - an increase in precipitation def
Autorzy: , .
Tytuł czasopisma:
Seria: 003The Meteorological Conditions of Precipitation Deficits in the Cultivation of Winter Wheat in Central and Eastern PolandJournal of Ecological Engineering20232299-89932022/202310.12911/22998993/168349Baranowska, Alicjaair temperatureWpływ czynników środowiskowych i agrotechnicznych na cechy jakościowe i plonowanie wybranych gatunków roślinFINAL_PUBLISHEDThe problem of precipitation deficits constitutes an issue that is significant on a global, re-gional, and local scale, particularly in the aspect of climate warming. The purpose of this research was to determine the amount, frequency and trends of precipitation deficits in the cultivation of winter wheat in central and eastern Poland, over a period of fifty years (from 1971 to 2020). This study used the values of average monthly air temperatures, as well as monthly total precipitation, decadal precipitation needs of winter wheat within central and eastern Poland. Based on the performed research, both spatial and temporal differences were observed in the scope of the amount and frequency of precipitation deficits in the cultivation of winter wheat. The lowest risk of precipitation deficits was found in May (from 15% to 32%), which is a critical month in the cultivation of this plant in Poland, while the highest risk of precipitation deficits was observed in June (from 22% to 56%), which is an unfavourable phenomenon, because winter wheat is in the so-called grain filling phase since mid-June. It was also found that there , Q, 003, Vol. 24, 2081-139X, Fundusz Rozwoju Nauki PSW, CC-BY, 2023-08-16, 10:09, issue 9, x, PB/26/2020, AT_PUBLICATION ; 2023-09-18, 12:23 ; p. 50--62, 2299-8993, 3122889230, OPEN_JOURNAL, 3121869016
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Praca recenzowana
Słowa kluczowe ang.: he problem of precipitation deficits constitutes an issue that is significant on a global, re-gional, and local scale, particularly in the aspect of climate warming. The purpose of this research was to determine the amount, frequency and trends of precipitation deficits in the cultivation of winter wheat in central and eastern Poland, over a period of fifty years (from 1971 to 2020). This study used the values of average monthly air temperatures, as well as monthly total precipitation, decadal precipitation needs of winter wheat within central and eastern Poland. Based on the performed research, both spatial and temporal differences were observed in the scope of the amount and frequency of precipitation deficits in the cultivation of winter wheat. The lowest risk of precipitation deficits was found in May (from 15% to 32%), which is a critical month in the cultivation of this plant in Poland, while the highest risk of precipitation deficits was observed in June (from 22% to 56%), which is an unfavourable phenomenon, because winter wheat is in the so-called grain filling phase since mid-June. It was also found that there is a statistically significant upward trend of the winter wheat's precipitation needs in April, June, and July. An increase in the inflow of warm and dry air masses from the southern sectors was one of the factors impacting the amount and frequency of precipitation deficits in the cultivation of wheat. The problem of climate warming that has been increasing in recent years, and - as a consequence - an increase in precipitation deficit during the growing season of plants, demonstrate the need for further research in this scope.^aatmospheric circulation^aLublin Region^aprecipitation deficits^atotal precipitation^awinter wheat
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Nr opisu: stations were used in the study. The assessment of spatiotemporal variation in atmospheric drought in the study area was based on calculations of the aridity index. The analysis showed an increase in the severity of atmospheric drought in the Lublin region, with intensification of this phenomenon in the last two decades, especially in the warmer half of the year (April, June-August). The main cause of drought in the Lublin region was identified as a statistically significant increase in air temperature (on average, from 0.4 °C to 0.7 °C/10 years in April, July and August, and from 0.2 °C to 0.5 °C/10 years in June) together with the absence of changes in precipitation in the warmer half of the year. This may be linked to some increase in the frequency of high-pressure circulation types, both non-directional and advection from the south. Due to the worsening problem of drought in Poland in recent years, especially in agriculture, there is a need for further research on this subject and for solutions aimed at optimizing agricultural use of the productive environment.^aair temperature^aaridity index A^aatmospheric circulation^adrought^aprecipitation totals^aLublin Region
Autorzy: .
Tytuł pracy: Spatiotemporal Assessment and Meteorological Determinants of Atmospheric Drought in Agricultural Areas of East-Central PolandAgronomy20212073-43952021/202210.3390/agronomy11122405Baranowska, AlicjaagricultureWpływ czynników środowiskowych i agrotechnicznych na cechy jakościowe i plonowanie wybranych gatunków roślinFINAL_PUBLISHEDAtmospheric drought is an extremely important issue on a global, regional and local scale, especially in the context of climate change. The aim of the study was to assess the spatiotemporal variation of atmospheric (meteorological) drought in agricultural areas of east-central Poland, represented by the Lublin Voivodeship (Lublin region) in 1971-2015. Average monthly air temperatures and monthly precipitation totals recorded over the 45-year period at 25 weather stations were used in the study. The assessment of spatiotemporal variation in atmospheric drought in the study area was based on calculations of the aridity index. The analysis showed an increase in the severity of atmospheric drought in the Lublin region, with intensification of this phenomenon in the last two decades, especially in the warmer half of the year (April, June-August). The main cause of drought in the Lublin region was identified as a statistically significant increase in air temperature (on average, from 0.4 °C to 0.7 °C/10 years in April, July and August, and from 0.2 °C to 0.5 °C/10 years in June) together with the absence of changes in precipitation in the warmer half of the year. This may be linked to some increase in the frequency of high-pressure circulation types, both non-directional and advection from the south. Due to the worsening problem of drought in Poland in recent years, especially in agriculture, there is a need for further research on this subject and for solutions aimed at optimizing agricultural use of the productive environment.air temperaturearidity index Aatmospheric circulationdroughtprecipitation totalsLublin Region : Vol. 11 : Fundusz Rozwoju Nauki PSW : CC-BY, OPEN_JOURNAL, 3129018995
Tytuł pracy:
Charakterystyka formalna: weather stations were used in the study. The assessment of spatiotemporal variation in atmospheric drought in the study area was based on calculations of the aridity index. The analysis showed an increase in the severity of atmospheric drought in the Lublin region, with intensification of this phenomenon in the last two decades, especially in the warmer half of the year (April, June-August). The main cause of drought in the Lublin region was identified as a statistically significant increase in air temperature (on average, from 0.4 °C to 0.7 °C/10 years in April, July and August, and from 0.2 °C to 0.5 °C/10 years in June) together with the absence of changes in precipitation in the warmer half of the year. This may be linked to some increase in the frequency of high-pressure circulation types, both non-directional and advection from the south. Due to the worsening problem of drought in Poland in recent years, especially in agriculture, there is a need for further research on this subject and for solutions aimed at optimizing agricultural use of the productive environment.^aair temperature^aaridity index A^aatmospheric circulation^adrought^aprecipitation totals^aLublin Region
Słowa kluczowe ang.: stations were used in the study. The assessment of spatiotemporal variation in atmospheric drought in the study area was based on calculations of the aridity index. The analysis showed an increase in the severity of atmospheric drought in the Lublin region, with intensification of this phenomenon in the last two decades, especially in the warmer half of the year (April, June-August). The main cause of drought in the Lublin region was identified as a statistically significant increase in air temperature (on average, from 0.4 °C to 0.7 °C/10 years in April, July and August, and from 0.2 °C to 0.5 °C/10 years in June) together with the absence of changes in precipitation in the warmer half of the year. This may be linked to some increase in the frequency of high-pressure circulation types, both non-directional and advection from the south. Due to the worsening problem of drought in Poland in recent years, especially in agriculture, there is a need for further research on this subject and for solutions aimed at optimizing agricultural use of the productive environment.^aair temperature^aaridity index A^aatmospheric circulation^adrought^aprecipitation totals^aLublin Region
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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
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