Standard

Exceptional atmospheric circulation during the "Dust Bowl". / Broennimann, S.; Stickler, A.; Griesser, T.; Ewen, T.; Grant, A. N.; Fischer, A. M.; Schraner, M.; Peter, T.; Rozanov, E.; Ross, T.

в: Geophysical Research Letters, Том 36, 08802, 16.04.2009.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Broennimann, S, Stickler, A, Griesser, T, Ewen, T, Grant, AN, Fischer, AM, Schraner, M, Peter, T, Rozanov, E & Ross, T 2009, 'Exceptional atmospheric circulation during the "Dust Bowl"', Geophysical Research Letters, Том. 36, 08802. https://doi.org/10.1029/2009GL037612

APA

Broennimann, S., Stickler, A., Griesser, T., Ewen, T., Grant, A. N., Fischer, A. M., Schraner, M., Peter, T., Rozanov, E., & Ross, T. (2009). Exceptional atmospheric circulation during the "Dust Bowl". Geophysical Research Letters, 36, [08802]. https://doi.org/10.1029/2009GL037612

Vancouver

Broennimann S, Stickler A, Griesser T, Ewen T, Grant AN, Fischer AM и пр. Exceptional atmospheric circulation during the "Dust Bowl". Geophysical Research Letters. 2009 Апр. 16;36. 08802. https://doi.org/10.1029/2009GL037612

Author

Broennimann, S. ; Stickler, A. ; Griesser, T. ; Ewen, T. ; Grant, A. N. ; Fischer, A. M. ; Schraner, M. ; Peter, T. ; Rozanov, E. ; Ross, T. / Exceptional atmospheric circulation during the "Dust Bowl". в: Geophysical Research Letters. 2009 ; Том 36.

BibTeX

@article{cdf388b0d2244351a9a9099138cb6126,
title = "Exceptional atmospheric circulation during the {"}Dust Bowl{"}",
abstract = "The three-dimensional, regional and large-scale atmospheric circulation during the {"}Dust Bowl{"} is analyzed based on newly available historical upper-air data and reconstructed upper-level fields. The Great Plains Low Level Jet, transporting moisture into the region, was weakened on its eastern side, shallower, and penetrated less far north than during wet years. Nocturnal convection was likely suppressed by increased stability. Strong mid-tropospheric ridging was found over the Great Plains, and upper-tropospheric flow anomalies extended from the North Pacific across North America to the Atlantic. These findings provide a dynamical view of the {"}Dust Bowl{"} droughts, some aspects of which are distinct from other droughts. It is demonstrated that this is important for assessing predictive capabilities of current modeling systems. Citation: Bronnimann, S., A. Stickler, T. Griesser, T. Ewen, A. N. Grant, A. M. Fischer, M. Schraner, T. Peter, E. Rozanov, and T. Ross (2009), Exceptional atmospheric circulation during the {"}Dust Bowl,{"} Geophys. Res. Lett., 36, L08802, doi:10.1029/2009GL037612.",
keywords = "LOW-LEVEL JET, CHEMISTRY-CLIMATE MODEL, NORTH-AMERICAN DROUGHT, CENTRAL UNITED-STATES, GREAT-PLAINS, HEAT WAVES, VARIABILITY, SUMMER, TRANSPORT, MOISTURE",
author = "S. Broennimann and A. Stickler and T. Griesser and T. Ewen and Grant, {A. N.} and Fischer, {A. M.} and M. Schraner and T. Peter and E. Rozanov and T. Ross",
year = "2009",
month = apr,
day = "16",
doi = "10.1029/2009GL037612",
language = "Английский",
volume = "36",
journal = "Geophysical Research Letters",
issn = "0094-8276",
publisher = "American Geophysical Union",

}

RIS

TY - JOUR

T1 - Exceptional atmospheric circulation during the "Dust Bowl"

AU - Broennimann, S.

AU - Stickler, A.

AU - Griesser, T.

AU - Ewen, T.

AU - Grant, A. N.

AU - Fischer, A. M.

AU - Schraner, M.

AU - Peter, T.

AU - Rozanov, E.

AU - Ross, T.

PY - 2009/4/16

Y1 - 2009/4/16

N2 - The three-dimensional, regional and large-scale atmospheric circulation during the "Dust Bowl" is analyzed based on newly available historical upper-air data and reconstructed upper-level fields. The Great Plains Low Level Jet, transporting moisture into the region, was weakened on its eastern side, shallower, and penetrated less far north than during wet years. Nocturnal convection was likely suppressed by increased stability. Strong mid-tropospheric ridging was found over the Great Plains, and upper-tropospheric flow anomalies extended from the North Pacific across North America to the Atlantic. These findings provide a dynamical view of the "Dust Bowl" droughts, some aspects of which are distinct from other droughts. It is demonstrated that this is important for assessing predictive capabilities of current modeling systems. Citation: Bronnimann, S., A. Stickler, T. Griesser, T. Ewen, A. N. Grant, A. M. Fischer, M. Schraner, T. Peter, E. Rozanov, and T. Ross (2009), Exceptional atmospheric circulation during the "Dust Bowl," Geophys. Res. Lett., 36, L08802, doi:10.1029/2009GL037612.

AB - The three-dimensional, regional and large-scale atmospheric circulation during the "Dust Bowl" is analyzed based on newly available historical upper-air data and reconstructed upper-level fields. The Great Plains Low Level Jet, transporting moisture into the region, was weakened on its eastern side, shallower, and penetrated less far north than during wet years. Nocturnal convection was likely suppressed by increased stability. Strong mid-tropospheric ridging was found over the Great Plains, and upper-tropospheric flow anomalies extended from the North Pacific across North America to the Atlantic. These findings provide a dynamical view of the "Dust Bowl" droughts, some aspects of which are distinct from other droughts. It is demonstrated that this is important for assessing predictive capabilities of current modeling systems. Citation: Bronnimann, S., A. Stickler, T. Griesser, T. Ewen, A. N. Grant, A. M. Fischer, M. Schraner, T. Peter, E. Rozanov, and T. Ross (2009), Exceptional atmospheric circulation during the "Dust Bowl," Geophys. Res. Lett., 36, L08802, doi:10.1029/2009GL037612.

KW - LOW-LEVEL JET

KW - CHEMISTRY-CLIMATE MODEL

KW - NORTH-AMERICAN DROUGHT

KW - CENTRAL UNITED-STATES

KW - GREAT-PLAINS

KW - HEAT WAVES

KW - VARIABILITY

KW - SUMMER

KW - TRANSPORT

KW - MOISTURE

U2 - 10.1029/2009GL037612

DO - 10.1029/2009GL037612

M3 - статья

VL - 36

JO - Geophysical Research Letters

JF - Geophysical Research Letters

SN - 0094-8276

M1 - 08802

ER -

ID: 121288316