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The MeteoMet project - metrology for meteorology: challenges and results.

TLDR
The Metrology for Meteorology (MeteoMet) project as mentioned in this paper is an attempt to bridge the meteorological and metrological communities, which is the concept of traceability, an idea used in both fields but with a subtle difference in meaning.
Abstract
The study describes significant outcomes of the Metrology for Meteorology' project, MeteoMet, which is an attempt to bridge the meteorological and metrological communities. The concept of traceability, an idea used in both fields but with a subtle difference in meaning, is at the heart of the project. For meteorology, a traceable measurement is the one that can be traced back to a particular instrument, time and location. From a metrological perspective, traceability further implies that the measurement can be traced back to a primary realization of the quantity being measured in terms of the base units of the International System of Units, the SI. These two perspectives reflect long-standing differences in culture and practice and this project - and this study - represents only the first step towards better communication between the two communities. The 3 year MeteoMet project was funded by the European Metrology Research Program (EMRP) and involved 18 European National Metrological Institutes, 3 universities and 35 collaborating stakeholders including national meteorology organizations, research institutes, universities, associations and instrument companies. The project brought a metrological perspective to several long-standing measurement problems in meteorology and climatology, varying from conventional ground-based measurements to those made in the upper atmosphere. It included development and testing of novel instrumentation as well as improved calibration procedures and facilities, instrument intercomparison under realistic conditions and best practice dissemination. Additionally, the validation of historical temperature data series with respect to measurement uncertainties and a methodology for recalculation of the values were included.

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Machine learning for site-adaptation and solar radiation forecasting

TL;DR: Through a study case with real data, the benefits of using the proposed methodology based on machine and deep learning techniques to integrate data from different sources and to construct precise solar radiation forecasting models in regions where solar energy systems are required are shown.
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The altitudinal temperature lapse rates applied to high elevation rockfalls studies in the Western European Alps

TL;DR: In this paper, the authors quantify the values and the variability of the hourly altitudinal temperature lapse rates (ATLR) and apply this to estimated temperatures at high-elevation sites for rockfalls studies.
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New insights in the relation between climate and slope failures at high-elevation sites

TL;DR: In this article, the authors analyzed 358 slope failures which occurred in the Italian Alps in the period 2000-2016, at an elevation above 1500 m a.s. They used a statistical-based method to detect climate anomalies associated with the occurrence of slope failures, with the aim to catch an eventual climate signal in the preparation and/or triggering of the considered case studies.
References
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Journal ArticleDOI

The International Temperature Scale of 1990 (ITS-90)

TL;DR: The International Temperature Scale of 1990 as mentioned in this paper was adopted by the International Committee of Weights and Measures at its meeting in 1989, in accordance with the request embodied in Resolution 7 of the 18th General Conference of WEMS of 1987.
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Vapor Pressure Formulation for Water in Range 0 to 100 °C. A Revision.

TL;DR: A revision is made of that earlier formulation to make it consistent with the definitive experimental value of the vapor pressure of water at its triple point recently obtained by Guildner, Johnson, and Jones.
Journal ArticleDOI

The international temperature scale of 1990 (ITS-90)

TL;DR: The International Temperature Scale of 1990 (ITS-90) is introduced, and is operationally defined for different ranges from 0.65 K upwards in terms of vapour-pressure thermometers, gas thermometry, platinum resistance thermometry and optical pyrometry as mentioned in this paper.
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