About
25
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Introduction
Filippo Calì Quaglia is research fellow at INGV, Rome after completing a phd in polar sciences (aerosols and clouds) at the University Ca' Foscari, Venice. He worked at the Institute of Atmospheric Sciences and Climate ISAC, Italian National Research Council and participated in the 14th Italian/french expedition at Concordia Station, Antarctica, for 1 year and participated in various field campaigns also in Greenland, Svalbard Islands. Recently, he contributed to NASA ARCSIX campaigns.
Additional affiliations
September 2019 - August 2023
September 2020 - present
November 2017 - January 2019
Education
December 2014 - July 2017
September 2010 - December 2014
Publications
Publications (25)
Conducting fieldwork in polar regions presents a multifaceted challenge not only because of the remoteness of the environment, but also potential geopolitical disputes, language barriers, divergent national policies, and disparities in emergency healthcare access. This review addresses the climate crisis and reevaluates the ethical considerations o...
Measurements of spectral zenith radiance in the 320–950 nm wavelength range have been carried out since 2021 at the Thule High Arctic Atmospheric Observatory (THAAO,
https://www.thuleatmos-it.it/
, 76.5° N, 68.8° W, 225 m a.s.l) located in Pituffik, northern Greenland. This study evaluates whether such observations could provide, in principle, sci...
Ground-based high resolution observations of downward longwave irradiance (DLI), surface air temperature, water vapor surface partial pressure and column amount, zenith sky infrared (IR) radiance in the atmospheric window, and all-sky camera images are regularly obtained at the Thule High Arctic Atmospheric Observatory (THAAO, 76.5° N, 68.8° W), no...
The Arctic climate is influenced by the interaction of shortwave (SW) and longwave (LW) radiation with the atmosphere and the surface. The comprehensive evolution of the Surface Radiative Fluxes (SRF) on different time scales is of paramount importance to understanding the complex mechanisms governing the Arctic climate. However, only a few sites l...
Climate change is rapidly reshaping the research landscape in the polar regions. As such, Early Career Researchers (ECRs) face increasingly daunting challenges. In this opinion piece, we report on the challenges that early career researchers confront as they seek opportunities for professional development and career advancement in polar research in...
The relevance of the Arctic has become apparent in the last decades, and it is today widely agreed that this area is affected by fast and unavoidable changes taking place at the global and local scale. The Arctic environment is interesting from geopolitical, economic, and scientific perspectives, and the study of the natural components characterisi...
Ground-based high resolution observations of downward longwave irradiance (DLI), surface air temperature, water vapour surface partial pressure and column amount, zenith sky infrared (IR) radiance in the atmospheric window, and all-sky camera images are regularly obtained at the Thule High Arctic Atmospheric Observatory (THAAO, 76.5° N, 68.8° W), N...
The Arctic climate is influenced by the interaction of shortwave (SW) and longwave (LW) radiation with the atmosphere and the surface. The comprehensive evolution of the Surface Radiative Fluxes (SRF) on different time scales is of paramount importance to understanding the complex mechanisms governing the Arctic climate. However, only a few sites l...
Clouds are one of the key components of the Earth System still requiring further understanding. The complexity of the cloud itself and the different interactions with aerosol and radiation cause large uncertainties in the estimation of the cloud feedback in climate models. Processes involving clouds are particularly relevant at high latitudes, wher...
The Arctic radiative budget is strongly influenced by cloud variability and properties, and many processes of cloud formation-evolution-dissipation still require a more
extensive and deeper understanding. The spectral signature of clouds, i.e., the radiances, can be measured and used to discriminate the microphysics of clouds
(optical thickness, pa...
Boreal fires have increased during the last years and are projected to become more intense and frequent as a consequence of climate change. Wildfires produce a wide range of effects on the Arctic climate and ecosystem, and understanding these effects is crucial for predicting the future evolution of the Arctic region. This study focuses on the impa...
This study considers a set of state-of-the-art seasonal forecasting systems (ECMWF, MF, UKMO, CMCC, DWD and the corresponding multi-model ensemble) and quantifies their added value (if any) in predicting seasonal and monthly temperature and precipitation anomalies over the Mediterranean region compared to a simple forecasting method based on the ER...
Skill scores refer to the climatology ERA5 dataset as a reference Winter and summer starting date Calì Quaglia, F., Terzago, S., von Hardenberg, J., Temperature and precipitation seasonal forecasts over the Mediterranean region: added value compared to simple forecasting methods, Climate Dynamics, https://doi. Assessment of seasonal forecast skills...
Seasonal forecasts are increasingly employed as sources of information on the expected evolution of climate in the few months ahead by various end-users. This study provides an overall assessment of the skills of the main seasonal forecast systems available in the Copernicus Climate Data Store (C3S) in representing temperature and precipitation ano...
Extended and intense wildfires occurred in Northern Canada and, unexpectedly, on theGreenlandic West coast during summer 2017. The thick smoke plume emitted into theatmosphere was transported to the high Arctic, producing one of the largest impacts everobserved in the region. Evidence of Canadian and Greenlandic wildfires was recorded at the ThuleH...
Upward Longwave Irradiance Measured At The Ground During Project MACMAP 2020 2023 published 2021 in Istituto Nazionale di Geofisica e Vulcanologia (INGV)
Measurements of downward shortwave (SW) and longwave (LW) irradiance are collected by Kipp&Zonen CMP21 pyranometer and CGR4 pyrgeometer, respectively, installed on the roof of building 1971. Both...
Upward Shortwave Irradiance Measured At The Ground During Project MACMAP 2020 2023 published 2021 in Istituto Nazionale di Geofisica e Vulcanologia (INGV)
Measurements of downward shortwave (SW) and longwave (LW) irradiance are collected by Kipp&Zonen CMP21 pyranometer and CGR4 pyrgeometer, respectively, installed on the roof of building 1971. Both...
Pressure Temperature And Relative Humity At 4 M Above Ground published 2018 in Istituto Nazionale di Geofisica e Vulcanologia (INGV)
Measurements of Pressure (P, in kPa), Temperature (T, in °C), and Relative Humidity (RH, in %) carried out by means of a Campbell meteorological station installed at the Thule High Arctic Atmospheric Observatory, near...
Water Vapor Column Content Also Known As Integrated Water Vapor Or Precipitable Water Vapor published 2018 in Istituto Nazionale di Geofisica e Vulcanologia (INGV)
Measurements of integrated water vapor (IWV or PWV) at the Thule High Arctic Atmospheric Observatory (THAAO) carried out by means of a microwave spectrometer (VESPA-22) designed and buil...
Measurements of middle atmospheric water vapor mixing ratio vertical profiles at the Thule High Arctic Atmospheric Observatory (THAAO) carried out by means of a microwave spectrometer (VESPA-22) designed and built at the INGV laboratories in Rome. Measurements start in July 2016 and are carried out all year round. VESPA-22 measures the water vapor...
Surface ablation of the Greenland ice sheet is amplified by surface darkening caused by light-absorbing impurities such as mineral dust, black carbon, and pigmented microbial cells. We present the first quantitative assessment of the microbial contribution to the ice sheet surface darkening, based on field measurements of surface reflectance and co...
Understanding climate variability and change demands for the assessment of extremes in climate such as cold spells, heat waves, intense precipitation among others. This thesis analyses the output of the EC-Earth Global Climate Model (GCM) run at different spatial resolutions, from about � 125 km to �16 km, over the European domain to assess the imp...