Evaluation of regional climate models ALARO-0 and REMO2015 at 0.22° resolution over the CORDEX Central Asia domain
To allow for climate impact studies on human and natural systems, high-resolution climate information is needed. Over some parts of the world plenty of regional climate simulations have been carried out, while in other regions hardly any high-resolution climate information is available. The CORDEX C...
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Veröffentlicht in: | Geoscientific Model Development 2021-03, Vol.14 (3), p.1267-1293 |
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Zusammenfassung: | To allow for climate impact studies on human and natural systems,
high-resolution climate information is needed. Over some parts of the world
plenty of regional climate simulations have been carried out, while in other
regions hardly any high-resolution climate information is available. The CORDEX
Central Asia domain is one of these regions, and this article describes the
evaluation for two regional climate models (RCMs), REMO and ALARO-0, that
were run for the first time at a horizontal resolution of 0.22∘
(25 km) over this region. The output of the ERA-Interim-driven RCMs is
compared with different observational datasets over the 1980–2017 period.
REMO scores better for temperature, whereas the ALARO-0 model
prevails for precipitation. Studying specific subregions provides deeper
insight into the strengths and weaknesses of both RCMs over the CAS-CORDEX
domain. For example, ALARO-0 has difficulties in simulating the temperature
over the northern part of the domain, particularly when snow cover is
present, while REMO poorly simulates the annual cycle of precipitation over
the Tibetan Plateau. The evaluation of minimum and maximum temperature
demonstrates that both models underestimate the daily temperature range.
This study aims to evaluate whether REMO and ALARO-0 provide reliable
climate information over the CAS-CORDEX domain for impact modeling and
environmental assessment applications. Depending on the evaluated season and variable, it is demonstrated that the produced climate data can be used in several subregions, e.g., temperature and precipitation over western Central Asia in autumn. At the same time, a bias adjustment is required for regions
where significant biases have been identified. |
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ISSN: | 1991-9603 1991-959X 1991-962X 1991-9603 1991-962X |
DOI: | 10.5194/gmd-14-1267-2021 |