Temporal and spatial scaling impacts on extreme precipitation

Publikation: Beiträge in ZeitschriftenZeitschriftenaufsätzeForschungbegutachtet

Standard

Temporal and spatial scaling impacts on extreme precipitation. / Eggert, Bastian; Berg, Peter; Haerter, Jan Olaf et al.
in: Atmospheric Chemistry and Physics, Jahrgang 15, Nr. 10, 29.05.2015, S. 5957-5971.

Publikation: Beiträge in ZeitschriftenZeitschriftenaufsätzeForschungbegutachtet

Harvard

Eggert, B, Berg, P, Haerter, JO, Jacob, D & Moseley, C 2015, 'Temporal and spatial scaling impacts on extreme precipitation', Atmospheric Chemistry and Physics, Jg. 15, Nr. 10, S. 5957-5971. https://doi.org/10.5194/acp-15-5957-2015

APA

Eggert, B., Berg, P., Haerter, J. O., Jacob, D., & Moseley, C. (2015). Temporal and spatial scaling impacts on extreme precipitation. Atmospheric Chemistry and Physics, 15(10), 5957-5971. https://doi.org/10.5194/acp-15-5957-2015

Vancouver

Eggert B, Berg P, Haerter JO, Jacob D, Moseley C. Temporal and spatial scaling impacts on extreme precipitation. Atmospheric Chemistry and Physics. 2015 Mai 29;15(10):5957-5971. doi: 10.5194/acp-15-5957-2015

Bibtex

@article{2dcfc3eb87a64d45adbdebe9c36e7388,
title = "Temporal and spatial scaling impacts on extreme precipitation",
abstract = "Convective and stratiform precipitation events have fundamentally different physical causes. Using a radar composite over Germany, this study separates these precipitation types and compares extremes at different spatial and temporal scales, ranging from 1 to 50 km and 5 min to 6 h, respectively. Four main objectives are addressed. First, we investigate extreme precipitation intensities for convective and stratiform precipitation events at different spatial and temporal resolutions to identify type-dependent space and time reduction factors and to analyze regional and seasonal differences over Germany. We find strong differences between the types, with up to 30% higher reduction factors for convective compared to stratiform extremes, exceeding all other observed seasonal and regional differences within one type. Second, we investigate how the differences in reduction factors affect the contribution of each type to extreme events as a whole, again dependent on the scale and the threshold chosen. A clear shift occurs towards more convective extremes at higher resolution or higher percentiles. For horizontal resolutions of current climate model simulations, i.e., ∼10 km, the temporal resolution of the data as well as the chosen threshold have profound influence on which type of extreme will be statistically dominant. Third, we compare the ratio of area to duration reduction factor for convective and stratiform events and find that convective events have lower effective advection velocities than stratiform events and are therefore more strongly affected by spatial than by temporal aggregation. Finally, we discuss the entire precipitation distribution regarding data aggregation and identify matching pairs of temporal and spatial resolutions where similar distributions are observed. The information is useful for planning observational networks or storing model data at different temporal and spatial scales.",
keywords = "Environmental Governance",
author = "Bastian Eggert and Peter Berg and Haerter, {Jan Olaf} and Daniela Jacob and Christopher Moseley",
note = "Publisher Copyright: {\textcopyright} Author(s) 2015.",
year = "2015",
month = may,
day = "29",
doi = "10.5194/acp-15-5957-2015",
language = "English",
volume = "15",
pages = "5957--5971",
journal = "Atmospheric Chemistry and Physics",
issn = "1680-7316",
publisher = "Copernicus Publications",
number = "10",

}

RIS

TY - JOUR

T1 - Temporal and spatial scaling impacts on extreme precipitation

AU - Eggert, Bastian

AU - Berg, Peter

AU - Haerter, Jan Olaf

AU - Jacob, Daniela

AU - Moseley, Christopher

N1 - Publisher Copyright: © Author(s) 2015.

PY - 2015/5/29

Y1 - 2015/5/29

N2 - Convective and stratiform precipitation events have fundamentally different physical causes. Using a radar composite over Germany, this study separates these precipitation types and compares extremes at different spatial and temporal scales, ranging from 1 to 50 km and 5 min to 6 h, respectively. Four main objectives are addressed. First, we investigate extreme precipitation intensities for convective and stratiform precipitation events at different spatial and temporal resolutions to identify type-dependent space and time reduction factors and to analyze regional and seasonal differences over Germany. We find strong differences between the types, with up to 30% higher reduction factors for convective compared to stratiform extremes, exceeding all other observed seasonal and regional differences within one type. Second, we investigate how the differences in reduction factors affect the contribution of each type to extreme events as a whole, again dependent on the scale and the threshold chosen. A clear shift occurs towards more convective extremes at higher resolution or higher percentiles. For horizontal resolutions of current climate model simulations, i.e., ∼10 km, the temporal resolution of the data as well as the chosen threshold have profound influence on which type of extreme will be statistically dominant. Third, we compare the ratio of area to duration reduction factor for convective and stratiform events and find that convective events have lower effective advection velocities than stratiform events and are therefore more strongly affected by spatial than by temporal aggregation. Finally, we discuss the entire precipitation distribution regarding data aggregation and identify matching pairs of temporal and spatial resolutions where similar distributions are observed. The information is useful for planning observational networks or storing model data at different temporal and spatial scales.

AB - Convective and stratiform precipitation events have fundamentally different physical causes. Using a radar composite over Germany, this study separates these precipitation types and compares extremes at different spatial and temporal scales, ranging from 1 to 50 km and 5 min to 6 h, respectively. Four main objectives are addressed. First, we investigate extreme precipitation intensities for convective and stratiform precipitation events at different spatial and temporal resolutions to identify type-dependent space and time reduction factors and to analyze regional and seasonal differences over Germany. We find strong differences between the types, with up to 30% higher reduction factors for convective compared to stratiform extremes, exceeding all other observed seasonal and regional differences within one type. Second, we investigate how the differences in reduction factors affect the contribution of each type to extreme events as a whole, again dependent on the scale and the threshold chosen. A clear shift occurs towards more convective extremes at higher resolution or higher percentiles. For horizontal resolutions of current climate model simulations, i.e., ∼10 km, the temporal resolution of the data as well as the chosen threshold have profound influence on which type of extreme will be statistically dominant. Third, we compare the ratio of area to duration reduction factor for convective and stratiform events and find that convective events have lower effective advection velocities than stratiform events and are therefore more strongly affected by spatial than by temporal aggregation. Finally, we discuss the entire precipitation distribution regarding data aggregation and identify matching pairs of temporal and spatial resolutions where similar distributions are observed. The information is useful for planning observational networks or storing model data at different temporal and spatial scales.

KW - Environmental Governance

UR - http://www.scopus.com/inward/record.url?scp=84927760048&partnerID=8YFLogxK

U2 - 10.5194/acp-15-5957-2015

DO - 10.5194/acp-15-5957-2015

M3 - Journal articles

AN - SCOPUS:84927760048

VL - 15

SP - 5957

EP - 5971

JO - Atmospheric Chemistry and Physics

JF - Atmospheric Chemistry and Physics

SN - 1680-7316

IS - 10

ER -

DOI

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