Projected changes to extreme freezing precipitation and design ice loads over North America based on a large ensemble of Canadian regional climate model simulations
<p>Atmospheric ice accretion caused by freezing precipitation (FP) can lead to severe damage and the failure of buildings and infrastructure. This study investigates projected changes to extreme ice loads – those used to design infrastructure over North America (NA) – for future periods of spe...
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2019-04-01
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doaj-e26d3fc0819a497ea549554fd42cffcc2020-11-25T00:36:31ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812019-04-011985787210.5194/nhess-19-857-2019Projected changes to extreme freezing precipitation and design ice loads over North America based on a large ensemble of Canadian regional climate model simulationsD. I. Jeong0A. J. Cannon1X. Zhang2Climate Research Division, Environment and Climate Change Canada, Toronto, Ontario, M3H 5T4, CanadaClimate Research Division, Environment and Climate Change Canada, Victoria, British Columbia, V8W 2Y2, CanadaClimate Research Division, Environment and Climate Change Canada, Toronto, Ontario, M3H 5T4, Canada<p>Atmospheric ice accretion caused by freezing precipitation (FP) can lead to severe damage and the failure of buildings and infrastructure. This study investigates projected changes to extreme ice loads – those used to design infrastructure over North America (NA) – for future periods of specified global mean temperature change (GMTC), relative to the recent 1986–2016 period, using a large 50-member initial-condition ensemble of the CanRCM4 regional climate model, driven by CanESM2 under the RCP8.5 scenario. The analysis is based on 3-hourly ice accretions on horizontal, vertical and radial surfaces calculated based on FP diagnosed by the offline Bourgouin algorithm and wind speed during FP. The CanRCM4 ensemble projects an increase in future design ice loads for most of northern NA and decreases for most of southern NA and some northeastern coastal regions. These changes are mainly caused by regional increases in future upper-level and surface temperatures associated with global warming. Projected changes in design ice thickness are also affected by changes in future precipitation intensity and surface wind speed. Changes in upper-level and surface temperature conditions for FP occurrence in CanRCM4 are in broad agreement with those from nine global climate models but display regional differences under the same level of global warming, indicating that a larger multi-model, multi-scenario ensemble may be needed to better account for additional sources of structural and scenario uncertainty. Increases in ice accretion for latitudes higher than 40<span class="inline-formula"><sup>∘</sup></span> N are substantial and would have clear implications for future building and infrastructure design.</p>https://www.nat-hazards-earth-syst-sci.net/19/857/2019/nhess-19-857-2019.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
D. I. Jeong A. J. Cannon X. Zhang |
spellingShingle |
D. I. Jeong A. J. Cannon X. Zhang Projected changes to extreme freezing precipitation and design ice loads over North America based on a large ensemble of Canadian regional climate model simulations Natural Hazards and Earth System Sciences |
author_facet |
D. I. Jeong A. J. Cannon X. Zhang |
author_sort |
D. I. Jeong |
title |
Projected changes to extreme freezing precipitation and design ice loads over North America based on a large ensemble of Canadian regional climate model simulations |
title_short |
Projected changes to extreme freezing precipitation and design ice loads over North America based on a large ensemble of Canadian regional climate model simulations |
title_full |
Projected changes to extreme freezing precipitation and design ice loads over North America based on a large ensemble of Canadian regional climate model simulations |
title_fullStr |
Projected changes to extreme freezing precipitation and design ice loads over North America based on a large ensemble of Canadian regional climate model simulations |
title_full_unstemmed |
Projected changes to extreme freezing precipitation and design ice loads over North America based on a large ensemble of Canadian regional climate model simulations |
title_sort |
projected changes to extreme freezing precipitation and design ice loads over north america based on a large ensemble of canadian regional climate model simulations |
publisher |
Copernicus Publications |
series |
Natural Hazards and Earth System Sciences |
issn |
1561-8633 1684-9981 |
publishDate |
2019-04-01 |
description |
<p>Atmospheric ice accretion caused by freezing precipitation (FP) can lead to severe damage and the
failure of buildings and infrastructure. This study investigates projected
changes to extreme ice loads – those used to design infrastructure over
North America (NA) – for future periods of specified global mean temperature
change (GMTC), relative to the recent 1986–2016 period, using a large
50-member initial-condition ensemble of the CanRCM4 regional climate model,
driven by CanESM2 under the RCP8.5 scenario. The analysis is based on
3-hourly ice accretions on horizontal, vertical and radial surfaces
calculated based on FP diagnosed by the offline Bourgouin algorithm and wind
speed during FP. The CanRCM4 ensemble projects an increase in future design
ice loads for most of northern NA and decreases for most of southern NA and
some northeastern coastal regions. These changes are mainly caused by
regional increases in future upper-level and surface temperatures associated
with global warming. Projected changes in design ice thickness are also
affected by changes in future precipitation intensity and surface wind speed.
Changes in upper-level and surface temperature conditions for FP occurrence
in CanRCM4 are in broad agreement with those from nine global climate models
but display regional differences under the same level of global warming,
indicating that a larger multi-model, multi-scenario ensemble may be needed
to better account for additional sources of structural and scenario
uncertainty. Increases in ice accretion for latitudes higher than
40<span class="inline-formula"><sup>∘</sup></span> N are substantial and would have clear implications for future
building and infrastructure design.</p> |
url |
https://www.nat-hazards-earth-syst-sci.net/19/857/2019/nhess-19-857-2019.pdf |
work_keys_str_mv |
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