Effects of the North Atlantic Oscillation on precipitation-type frequency and distribution in the eastern United States
Summary The North Atlantic Oscillation (NAO) is the primary mode of atmospheric variability over the Atlantic Ocean and plays an important role in climate variability over eastern North America. The frequency of extreme climate events and the associated social and economic impacts is also tied to th...
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| Autor*in: |
Durkee, J. D. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2007 |
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| Systematik: |
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| Anmerkung: |
© Springer-Verlag 2007 |
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| Übergeordnetes Werk: |
Enthalten in: Theoretical and applied climatology - Springer-Verlag, 1986, 94(2007), 1-2 vom: 23. Okt., Seite 51-65 |
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| Übergeordnetes Werk: |
volume:94 ; year:2007 ; number:1-2 ; day:23 ; month:10 ; pages:51-65 |
| Links: |
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| DOI / URN: |
10.1007/s00704-007-0345-x |
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| Katalog-ID: |
OLC2048441785 |
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| 245 | 1 | 0 | |a Effects of the North Atlantic Oscillation on precipitation-type frequency and distribution in the eastern United States |
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| 520 | |a Summary The North Atlantic Oscillation (NAO) is the primary mode of atmospheric variability over the Atlantic Ocean and plays an important role in climate variability over eastern North America. The frequency of extreme climate events and the associated social and economic impacts is also tied to the strength and phase of the NAO. In this study, seasonal phases of the NAO are compared to changes in the frequency and distribution of winter season (December–March) precipitation-type observations for the years 1961–2001 in the eastern U.S. Statistically significant increases in the frequency of rain observations across the study region are associated with positive NAO phases. Additionally, significant increases in the occurrence of snow are confined to the northern portion of the eastern U.S. during positive NAO phases. Connections between the phase of the NAO and the prevailing synoptic-scale circulation, at least partially, explain the inter-seasonal distribution of precipitation types across the eastern U.S. Using an intra-seasonal or intra-monthly NAO index may reveal a more robust relationship between snowfall observations across the eastern U.S. and surface pressure variability over the North Atlantic. | ||
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10.1007/s00704-007-0345-x doi (DE-627)OLC2048441785 (DE-He213)s00704-007-0345-x-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Durkee, J. D. verfasserin aut Effects of the North Atlantic Oscillation on precipitation-type frequency and distribution in the eastern United States 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Summary The North Atlantic Oscillation (NAO) is the primary mode of atmospheric variability over the Atlantic Ocean and plays an important role in climate variability over eastern North America. The frequency of extreme climate events and the associated social and economic impacts is also tied to the strength and phase of the NAO. In this study, seasonal phases of the NAO are compared to changes in the frequency and distribution of winter season (December–March) precipitation-type observations for the years 1961–2001 in the eastern U.S. Statistically significant increases in the frequency of rain observations across the study region are associated with positive NAO phases. Additionally, significant increases in the occurrence of snow are confined to the northern portion of the eastern U.S. during positive NAO phases. Connections between the phase of the NAO and the prevailing synoptic-scale circulation, at least partially, explain the inter-seasonal distribution of precipitation types across the eastern U.S. Using an intra-seasonal or intra-monthly NAO index may reveal a more robust relationship between snowfall observations across the eastern U.S. and surface pressure variability over the North Atlantic. North Atlantic Oscillation Data Range North Atlantic Oscillation Index Precipitation Type North Atlantic Oscillation Phase Frye, J. D. aut Fuhrmann, C. M. aut Lacke, M. C. aut Jeong, H. G. aut Mote, T. L. aut Enthalten in Theoretical and applied climatology Springer-Verlag, 1986 94(2007), 1-2 vom: 23. Okt., Seite 51-65 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:94 year:2007 number:1-2 day:23 month:10 pages:51-65 https://doi.org/10.1007/s00704-007-0345-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_381 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4323 RA 1000 AR 94 2007 1-2 23 10 51-65 |
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10.1007/s00704-007-0345-x doi (DE-627)OLC2048441785 (DE-He213)s00704-007-0345-x-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Durkee, J. D. verfasserin aut Effects of the North Atlantic Oscillation on precipitation-type frequency and distribution in the eastern United States 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Summary The North Atlantic Oscillation (NAO) is the primary mode of atmospheric variability over the Atlantic Ocean and plays an important role in climate variability over eastern North America. The frequency of extreme climate events and the associated social and economic impacts is also tied to the strength and phase of the NAO. In this study, seasonal phases of the NAO are compared to changes in the frequency and distribution of winter season (December–March) precipitation-type observations for the years 1961–2001 in the eastern U.S. Statistically significant increases in the frequency of rain observations across the study region are associated with positive NAO phases. Additionally, significant increases in the occurrence of snow are confined to the northern portion of the eastern U.S. during positive NAO phases. Connections between the phase of the NAO and the prevailing synoptic-scale circulation, at least partially, explain the inter-seasonal distribution of precipitation types across the eastern U.S. Using an intra-seasonal or intra-monthly NAO index may reveal a more robust relationship between snowfall observations across the eastern U.S. and surface pressure variability over the North Atlantic. North Atlantic Oscillation Data Range North Atlantic Oscillation Index Precipitation Type North Atlantic Oscillation Phase Frye, J. D. aut Fuhrmann, C. M. aut Lacke, M. C. aut Jeong, H. G. aut Mote, T. L. aut Enthalten in Theoretical and applied climatology Springer-Verlag, 1986 94(2007), 1-2 vom: 23. Okt., Seite 51-65 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:94 year:2007 number:1-2 day:23 month:10 pages:51-65 https://doi.org/10.1007/s00704-007-0345-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_381 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4323 RA 1000 AR 94 2007 1-2 23 10 51-65 |
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10.1007/s00704-007-0345-x doi (DE-627)OLC2048441785 (DE-He213)s00704-007-0345-x-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Durkee, J. D. verfasserin aut Effects of the North Atlantic Oscillation on precipitation-type frequency and distribution in the eastern United States 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Summary The North Atlantic Oscillation (NAO) is the primary mode of atmospheric variability over the Atlantic Ocean and plays an important role in climate variability over eastern North America. The frequency of extreme climate events and the associated social and economic impacts is also tied to the strength and phase of the NAO. In this study, seasonal phases of the NAO are compared to changes in the frequency and distribution of winter season (December–March) precipitation-type observations for the years 1961–2001 in the eastern U.S. Statistically significant increases in the frequency of rain observations across the study region are associated with positive NAO phases. Additionally, significant increases in the occurrence of snow are confined to the northern portion of the eastern U.S. during positive NAO phases. Connections between the phase of the NAO and the prevailing synoptic-scale circulation, at least partially, explain the inter-seasonal distribution of precipitation types across the eastern U.S. Using an intra-seasonal or intra-monthly NAO index may reveal a more robust relationship between snowfall observations across the eastern U.S. and surface pressure variability over the North Atlantic. North Atlantic Oscillation Data Range North Atlantic Oscillation Index Precipitation Type North Atlantic Oscillation Phase Frye, J. D. aut Fuhrmann, C. M. aut Lacke, M. C. aut Jeong, H. G. aut Mote, T. L. aut Enthalten in Theoretical and applied climatology Springer-Verlag, 1986 94(2007), 1-2 vom: 23. Okt., Seite 51-65 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:94 year:2007 number:1-2 day:23 month:10 pages:51-65 https://doi.org/10.1007/s00704-007-0345-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_381 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4323 RA 1000 AR 94 2007 1-2 23 10 51-65 |
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10.1007/s00704-007-0345-x doi (DE-627)OLC2048441785 (DE-He213)s00704-007-0345-x-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Durkee, J. D. verfasserin aut Effects of the North Atlantic Oscillation on precipitation-type frequency and distribution in the eastern United States 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Summary The North Atlantic Oscillation (NAO) is the primary mode of atmospheric variability over the Atlantic Ocean and plays an important role in climate variability over eastern North America. The frequency of extreme climate events and the associated social and economic impacts is also tied to the strength and phase of the NAO. In this study, seasonal phases of the NAO are compared to changes in the frequency and distribution of winter season (December–March) precipitation-type observations for the years 1961–2001 in the eastern U.S. Statistically significant increases in the frequency of rain observations across the study region are associated with positive NAO phases. Additionally, significant increases in the occurrence of snow are confined to the northern portion of the eastern U.S. during positive NAO phases. Connections between the phase of the NAO and the prevailing synoptic-scale circulation, at least partially, explain the inter-seasonal distribution of precipitation types across the eastern U.S. Using an intra-seasonal or intra-monthly NAO index may reveal a more robust relationship between snowfall observations across the eastern U.S. and surface pressure variability over the North Atlantic. North Atlantic Oscillation Data Range North Atlantic Oscillation Index Precipitation Type North Atlantic Oscillation Phase Frye, J. D. aut Fuhrmann, C. M. aut Lacke, M. C. aut Jeong, H. G. aut Mote, T. L. aut Enthalten in Theoretical and applied climatology Springer-Verlag, 1986 94(2007), 1-2 vom: 23. Okt., Seite 51-65 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:94 year:2007 number:1-2 day:23 month:10 pages:51-65 https://doi.org/10.1007/s00704-007-0345-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_381 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4323 RA 1000 AR 94 2007 1-2 23 10 51-65 |
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10.1007/s00704-007-0345-x doi (DE-627)OLC2048441785 (DE-He213)s00704-007-0345-x-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Durkee, J. D. verfasserin aut Effects of the North Atlantic Oscillation on precipitation-type frequency and distribution in the eastern United States 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Summary The North Atlantic Oscillation (NAO) is the primary mode of atmospheric variability over the Atlantic Ocean and plays an important role in climate variability over eastern North America. The frequency of extreme climate events and the associated social and economic impacts is also tied to the strength and phase of the NAO. In this study, seasonal phases of the NAO are compared to changes in the frequency and distribution of winter season (December–March) precipitation-type observations for the years 1961–2001 in the eastern U.S. Statistically significant increases in the frequency of rain observations across the study region are associated with positive NAO phases. Additionally, significant increases in the occurrence of snow are confined to the northern portion of the eastern U.S. during positive NAO phases. Connections between the phase of the NAO and the prevailing synoptic-scale circulation, at least partially, explain the inter-seasonal distribution of precipitation types across the eastern U.S. Using an intra-seasonal or intra-monthly NAO index may reveal a more robust relationship between snowfall observations across the eastern U.S. and surface pressure variability over the North Atlantic. North Atlantic Oscillation Data Range North Atlantic Oscillation Index Precipitation Type North Atlantic Oscillation Phase Frye, J. D. aut Fuhrmann, C. M. aut Lacke, M. C. aut Jeong, H. G. aut Mote, T. L. aut Enthalten in Theoretical and applied climatology Springer-Verlag, 1986 94(2007), 1-2 vom: 23. Okt., Seite 51-65 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:94 year:2007 number:1-2 day:23 month:10 pages:51-65 https://doi.org/10.1007/s00704-007-0345-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_381 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4323 RA 1000 AR 94 2007 1-2 23 10 51-65 |
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Effects of the North Atlantic Oscillation on precipitation-type frequency and distribution in the eastern United States |
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Summary The North Atlantic Oscillation (NAO) is the primary mode of atmospheric variability over the Atlantic Ocean and plays an important role in climate variability over eastern North America. The frequency of extreme climate events and the associated social and economic impacts is also tied to the strength and phase of the NAO. In this study, seasonal phases of the NAO are compared to changes in the frequency and distribution of winter season (December–March) precipitation-type observations for the years 1961–2001 in the eastern U.S. Statistically significant increases in the frequency of rain observations across the study region are associated with positive NAO phases. Additionally, significant increases in the occurrence of snow are confined to the northern portion of the eastern U.S. during positive NAO phases. Connections between the phase of the NAO and the prevailing synoptic-scale circulation, at least partially, explain the inter-seasonal distribution of precipitation types across the eastern U.S. Using an intra-seasonal or intra-monthly NAO index may reveal a more robust relationship between snowfall observations across the eastern U.S. and surface pressure variability over the North Atlantic. © Springer-Verlag 2007 |
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Summary The North Atlantic Oscillation (NAO) is the primary mode of atmospheric variability over the Atlantic Ocean and plays an important role in climate variability over eastern North America. The frequency of extreme climate events and the associated social and economic impacts is also tied to the strength and phase of the NAO. In this study, seasonal phases of the NAO are compared to changes in the frequency and distribution of winter season (December–March) precipitation-type observations for the years 1961–2001 in the eastern U.S. Statistically significant increases in the frequency of rain observations across the study region are associated with positive NAO phases. Additionally, significant increases in the occurrence of snow are confined to the northern portion of the eastern U.S. during positive NAO phases. Connections between the phase of the NAO and the prevailing synoptic-scale circulation, at least partially, explain the inter-seasonal distribution of precipitation types across the eastern U.S. Using an intra-seasonal or intra-monthly NAO index may reveal a more robust relationship between snowfall observations across the eastern U.S. and surface pressure variability over the North Atlantic. © Springer-Verlag 2007 |
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Summary The North Atlantic Oscillation (NAO) is the primary mode of atmospheric variability over the Atlantic Ocean and plays an important role in climate variability over eastern North America. The frequency of extreme climate events and the associated social and economic impacts is also tied to the strength and phase of the NAO. In this study, seasonal phases of the NAO are compared to changes in the frequency and distribution of winter season (December–March) precipitation-type observations for the years 1961–2001 in the eastern U.S. Statistically significant increases in the frequency of rain observations across the study region are associated with positive NAO phases. Additionally, significant increases in the occurrence of snow are confined to the northern portion of the eastern U.S. during positive NAO phases. Connections between the phase of the NAO and the prevailing synoptic-scale circulation, at least partially, explain the inter-seasonal distribution of precipitation types across the eastern U.S. Using an intra-seasonal or intra-monthly NAO index may reveal a more robust relationship between snowfall observations across the eastern U.S. and surface pressure variability over the North Atlantic. © Springer-Verlag 2007 |
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