Dario Camuffo

Prof. Dr. Dario Camuffo

Institute of Atmospheric Sciences & Climate, Consiglio Nazionale delle Ricerche, Rome, Lazio, Italy
orcid

Research Focus & Metrics

Academic Career Length

52Years (1975-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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3 July 2019 in Quarterly Journal of the Royal Meteorological Society
Verified
Journal Article
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LSLaura Slivinski
Laura Slivinski
GCGilbert P. Compo
Gilbert P. Compo
JWJeffrey S. Whitaker
Jeffrey S. Whitaker
PSPrashant D. Sardeshmukh
Prashant D. Sardeshmukh
BGBenjamin S. Giese
Benjamin S. Giese
PWPrzemysław Wyszyński
Przemysław Wyszyński
Historical reanalyses that span more than a century are needed for a wide range of studies, from understanding large‐scale climate trends to diagnosing the impacts of individual historical extreme weather events. The Twentieth Century Reanalysis (20CR) Project is an effort to fill this need. It is supported by the National Oceanic and Atmospheric Administration (NOAA), the Cooperative Institute for Research in Environmental Sciences (CIRES), and the U.S. Department of Energy (DOE), and is facilitated by collaboration with the international Atmospheric Circulation Reconstructions over the Earth initiative. 20CR is the first ensemble of sub‐daily global atmospheric conditions spanning over 100 years. This provides a best estimate of the weather at any given place and time as well as an estimate of its confidence and uncertainty. While extremely useful, version 2c of this dataset (20CRv2c) has several significant issues, including inaccurate estimates of confidence and a global sea level pressure bias in the mid‐19th century. These and other issues can reduce its effectiveness for studies at many spatial and temporal scales. Therefore, the 20CR system underwent a series of developments to generate a significant new version of the reanalysis. The version 3 system (NOAA‐CIRES‐DOE 20CRv3) uses upgraded data assimilation methods including an adaptive inflation algorithm; has a newer, higher‐resolution forecast model that specifies dry air mass; and assimilates a larger set of pressure observations. These changes have improved the ensemble‐based estimates of confidence, removed spin‐up effects in the precipitation fields, and diminished the sea‐level pressure bias. Other improvements include more accurate representations of storm intensity, smaller errors, and large‐scale reductions in model bias. The 20CRv3 system is comprehensively reviewed, focusing on the aspects that have ameliorated issues in 20CRv2c. Despite the many improvements, some challenges remain, including a systematic bias in tropical precipitation and time‐varying biases in southern high‐latitude pressure fields.

28 January 2016 in Environmental Research Letters
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JLJürg Luterbacher
Jürg Luterbacher
JWJohannes Werner
Johannes Werner
JSJ E Smerdon
J E Smerdon
LFL Fernández-Donado
L Fernández-Donado
FRFidel Rouco
Fidel Rouco
CZC Zerefos
C Zerefos

2 March 2010 in Climatic Change
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Rüdiger GlaserRüdiger Glaser
Rüdiger Glaser
DRDirk Riemann
Dirk Riemann
JSJohannes Schönbein
Johannes Schönbein
MBMariano Barriendos
Mariano Barriendos
RBRudolf Brázdil
Rudolf Brázdil
IHIso Himmelsbach
Iso Himmelsbach

1 April 2002 in Climatic Change
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Journal Article
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ZYZhongwei Yan
Zhongwei Yan
PJP. D. Jones
P. D. Jones
TDT. D. Davies
T. D. Davies
AMA. Moberg
A. Moberg
HBH. Bergström
H. Bergström
CYC. Yang
C. Yang

11 December 2015 in Heritage Science
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Johanna LeissnerJohanna Leissner
Johanna Leissner
RKRalf Kilian
Ralf Kilian
LKLola Kotova
Lola Kotova
DJDaniela Jacob
Daniela Jacob
UMUwe Mikolajewicz
Uwe Mikolajewicz
TVTomáš Vyhlídal
Tomáš Vyhlídal
Background: The present study reports results from the large-scale integrated EU project “Climate for Culture”. The full name, or title, of the project is Climate for Culture: damage risk assessment, economic impact and mitigation strategies for sustainable preservation of cultural heritage in times of climate change. This paper focusses on implementing high resolution regional climate models together with new building simulation tools in order to predict future outdoor and indoor climate conditions. The potential impact of gradual climate change on historic buildings and on the vast collections they contain has been assessed. Two moderate IPCC emission scenarios A1B and RCP 4.5 were used to predict indoor climates in historic buildings from the recent past until the year 2100. Risks to the building and to the interiors with valuable artifacts were assessed using damage functions. A set of generic building types based on data from existing buildings were used to transfer outdoor climate conditions to indoor conditions using high resolution climate projections for Europe and the Mediterranean. Results: The high resolution climate change simulations have been performed with the regional climate model REMO over the whole of Europe including the Mediterranean region. Whole building simulation tools and a simplified building model were developed for historic buildings; they were forced with high resolution climate simulations. This has allowed maps of future climate-induced risks for historic buildings and their interiors to be produced. With this procedure future energy demands for building control can also be calculated. Conclusion: With the newly developed method described here not only can outdoor risks for cultural heritage assets resulting from climate change be assessed, but also risks for indoor collections. This can be done for individual buildings as well as on a larger scale in the form of European risk maps. By using different standardized and exemplary artificial buildings in modelling climate change impact, a comparison between different regions in Europe has become possible for the first time. The methodology will serve heritage owners and managers as a decision tool, helping them to plan more effectively mitigation and adaption measures at various levels.

1 January 2001 in Atmospheric Environment
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Journal Article
Closed access
DCDario Camuffo
Dario Camuffo