RESULTS FROM 1 TO 20 OF 243

2023, Articolo in rivista, ITA

A vent'anni dal Lago Effimero (Ghiacciaio del Belvedere, Monte Rosa): eredità di un evento emblematico per le Alpi

Mortara G. (1, 2), Chiarle M. (1, 2), Tamburini A. (3, 2), Mercalli L. (4, 2), Cat Berro D. (4, 2)

L'articolo rievoca un momento particolare dell'evoluzione del Ghiacciaio del Belvedere (Gruppo del Monte Rosa, Alpi Occidentali Italiane) all'inizio degli anni 2000. Una rapida ed intensa "piena glaciale" ha provocato sorprendenti trasformazioni del ghiacciaio e la contestuale formazione di un grande lago epiglaciale (denominato "Lago Effimero"), che ha avviato una complessa operazione di protezione civile per ridurre il rischio di una piena improvvisa.

Nimbus (Torino) 90

2023, Rapporto di ricerca (Research report), ITA

Estate 2023: il raddoppio degli eventi di instabilità in alta quota è la nuova "normalità"

Marta Chiarle

Secondo le elaborazioni del Copernicus Climate Change Service, l'estate 2023 è stata nell'emisfero boreale la più calda dal 1940, superando di 0.66 °C la media del trentennio 1990-2020, già pienamente iscritto nel trend di riscaldamento climatico in atto a scala globale. Per quanto riguarda gli "effetti a terra", in Italia il 2023 sarà ricordato per la disastrosa alluvione di maggio in Emilia Romagna e per le drammatiche grandinate di luglio nel Nord Italia: l'occorrenza di questi eventi estremi ha definitivamente sgomberato il campo da possibili dubbi sul fatto che già oggi il cambiamento climatico stia avendo effetti incontrovertibili sul territorio e sulla nostra vita. In questo contesto, sono passati relativamente in sordina i numerosi eventi d'instabilità naturale occorsi anche quest'anno in alta quota nelle Alpi Italiane, una delle testimonianze più chiare di come l'ambiente naturale si stia riequilibrando alle mutate condizioni climatiche e ambientali.

2023, Articolo in rivista, ENG/ITA

Christmas Mass Movements in the Italian Alps

Marta Chiarle, Costanza Morino, Giovanni Mortara, Walter Alberto, Mario Ravello, Aristide Franchino, Giuseppe Orombelli, Marco Giardino, Luigi Perotti et Guido Nigrelli

Mass movements at high elevation during wintertime are rare events in the Italian Alps, but are generally large events compared to those occurring in other seasons. In a context of climate change, their interpretation is particularly challenging due to the risk implications during a highly tourist season in the mountains, and because their occurrence seemingly contradicts the attribution of recent mass movements in high-alpine environments to global warming. To shed some light on this topic, we reviewed 12 mass movements in the Italian Alps that occurred at elevations above 1500 m, documented from mid-December to January, henceforth during the Christmas period. The aim is to understand whether recent events may be related to ongoing climate and environmental changes. Even though the small number of analysed mass movements does not allow statistically based conclusions, some preliminary considerations could be drafted. We observe a seeming increase in the frequency and elevation of winter mass-movement events in the last two decades, with an increased number of failures involving rock slopes under permafrost conditions, and a transition from heavy-precipitations controlled mass movements to temperature-anomalies and -fluctuations controlled mass movements. We also show that any type of instability process can occur in winter, including debris flows, with rock falls/avalanches prevailing. These findings may partly stem from an increased number of mass-movement reports deriving from the growing attention in recent years to the impacts of climate change and their related risks. Considering the growing anthropic pressure on alpine areas even in winter, especially for tourism purposes, it is crucial to broaden our knowledge on winter mass movements by expanding and analysing a larger case history, through the opportunities offered by new technologies and citizen science.

Revue de géographie alpine (En ligne) 111 (2)

2023, Articolo in rivista, ENG/FRE

The Glaciated Slopes of the High Alpine Mountains: Holocene Evolution and Impacts of the Current Climate Crisis

Ludovic Ravanel, Melaine Le Roy, Florence Magnin, Marta Chiarle

After the wake-up calls of the summers of 2003 and 2015, along with their significant media impact, the succession of the summers of 2022 and 2023 represents a third stage and a clear acceleration in the warming and morphodynamics of the high Alpine mountains.

Revue de géographie alpine (En ligne) 111 (2)

2023, Rapporto di progetto (Project report), ITA

WP5 - Esportazione delle conoscenze a situazioni analoghe

Lorenzo Marchi, Enrico Marchese, Gianluca Marcato, Marco Cavalli, Marta Chiarle, Stefano Crema

Il WP5 è finalizzato alla definizione di un modello concettuale utilizzabile per trasferire gli approcci di analisi e le valutazioni conseguite nel bacino del rio Rotiano ad altri bacini idrografici della Provincia autonoma di Trento. Il WP5 si articola in tre attività: definizione di scenari di pericolosità residua, individuazione di situazioni potenzialmente critiche nel territorio provinciale e proposta di strategie di mitigazione.

2023, Articolo in rivista, ENG

1991-2020 climate normal in the European Alps: focus on high-elevation environments

Nigrelli G., Chiarle M.

Alps are an important geographical area of the European continent and, in this area, temperature increase is most evident. However, the 1991-2020 climate normal in the Alps has still not been thoroughly investigated. Aiming to fill this gap with a focus on high-elevation environments, minimum and maximum daily air temperature acquired by 23 automatic weather station were used. The results show that the mean annual values of minimum and maximum temperature for the 1991-2020 climate normal in the Alps are -2.4°C and 4.4°C, respectively, with a warming rate of 0.5°C/10 years. The mean annual temperature comparison between 1961-1990 and 1971-2000, 1961-1990 and 1981-2010, 1961-1990 and 1991-2020 climate normal show an increase of 0.3°C, 0.5°C and 0.9°C, respectively. The results also confirm that seasonal and annual temperatures are rising through the whole Alpine arc, mainly in summer and autumn. This work highlights that annual minimum and maximum temperature do not seem to be affected by a positive elevation-dependent warming. Instead, a positive elevation-dependent warming in the maximum values of the annual minimum temperature was found. If anthropogenic emissions maintain the trend of the last decades, the expected mean annual temperature of the 2001-2030 climate normal is -0.2°C, with an increase of 0.5°C if compared to the 1991-2020 climate normal and with an increase of 1.5°C if compared to the 1961-1990 climate normal. This study highlights the warming rate that is now present in the European Alps, provides indications on the warming rate that will occur in the coming years and highlights the importance of carrying out investigations that consider not only the last 30-year climate normal, but also the most recent 30-year climate normal by comparing them with each other.

Journal of Mountain Science 20 (8), pp. 2149–2163

DOI: 10.1007/s11629-023-7951-7

2023, Abstract in atti di convegno, ENG

The 2022 Marmolada Glacier failure in the framework of historical glacier instability in the Italian Alps

Chiarle M. (1), Viani C. (2), Mortara G. (1), Deline P. (3), Tamburini A. (4), Nigrelli G. (1)

26th Alpine Glaciological Meeting, Birmensdorf (CH), 09-10/02/2023

2022, Articolo in rivista, ENG

ANNUAL GLACIOLOGICAL SURVEY OF ITALIAN GLACIERS (2021) CAMPAGNA GLACIOLOGICA ANNUALE DEI GHIACCIAI ITALIANI (2021)

Baroni C.[1], Bondesan A.[2], Carturan L.[3], Chiarle M.[4], Scotti R.[5]

Baroni C., Bondesan A., Carturan L., Chiarle M. & Scotti R., Annual glaciological survey of Italian glaciers (2021). (IT ISSN 0391-9838, 2022).The annual glaciological survey (2021) conducted on Italian glaciers is here presented. About 200 volunteers operated last year in the three Alpine sectors (Piemonte -Valle d'Aosta, Lombardy and Triveneto) and in the Apennines (Calderone Glacier, Gran Sasso Group). One hundred and one glaciers were observed in the Piemonte -Valle d'Aosta sector while frontal variation was measured at the snout of fourty-nine glaciers. Twenty-seven and fifty-two glaciers were visited in the Lombardy Sector and in the Triveneto Sector, respectively (seventeen and fourty-four of which were measured, respectively). Data for seventeen Italian glaciers monitored during the 2020-2021 hydrological year are reported in the section on mass balance measurements: four glaciers in the Western Alps (Piemonte -Valle d'Aosta sector), twelve in the Eastern Alps (two in the Lombardy Sector, the other ten glaciers in the Triveneto Sector) and one in the Central Apennines).

Geografia fisica e dinamica quaternaria (Testo stamp.) 45 (1), pp. 69–167

DOI: 10.4461/GFDQ.2022.45.5

2022, Articolo in rivista, ENG

Large glacier failures in the Italian Alps over the last 90 years

Chiarle M. (1), Viani C. (2), Mortara G. (1), Deline P. (3), Tamburini A. (4) & Nigrelli G. (1)

Ice failures are among the least known and least studied mass movements, both because large events are quite rare, and because they usually develop in remote and little-frequented areas. However, the unprecedented transformation of glaciers due to climate change, on the one hand, and the growing human pressure on high-elevation environments, on the other, nowadays require a more careful and in-depth consideration of these hazardous processes, such as tragically highlighted by the collapse of the Marmolada Glacier (Italy) on July 3rd, 2022. In this context, a review of existing documentation on past glacier failures is essential for to learn about their spatio-temporal distribution, the characteristics of the glaciers where the failures occurred and flow properties. In turn, these findings are fundamental to inform the assessment of current and future hazards. The present work contributes to the topic by documenting, cataloguing, and analysing the glacier failures larger than 10,000 m3 that occurred in the Italian Alps in the period 1930-2022. 68 glacier failures are documented, which affected 29 glaciers distributed throughout the Italian Alps. The volumes of glacier failures are mostly between 10 000 and 50 000 m3 (1.1 x 106 m3 in one case). The events occurred mainly in summer, with a frequency peak in August. The H/L ratio, i.e. the ratio between the vertical (H) and horizontal (L) distances covered by the process, indicator of the mobility of the detached mass, is between 0.33 and 0.80. Although glacier failures can occur during both glacial advance and retreat, we found a sharp increase in the number of documented cases since the 1990s. We are aware that, due to the difficulty of finding information, the dataset provided in this work is only partially representative of the glacier failures that occurred in the Italian Alps in the period considered: nevertheless, it is a useful starting point for studies aimed at assessing hazards related to glacier failure, and for risk mitigation. Given the speed and intensity with which glaciers and their surrounding environments are evolving in response to climate change, their continuous observation is essential, as is the systematic documentation of glacier failure events. Remote sensing data and tools can nowadays facilitate glacier monitoring and the documentation of ice failures: however, field data such as those collected during the annual glaciological surveys of the Italian Glaciological Committee (CGI) remain fundamental for the validation of remote sensing data and numerical models.

Geografia fisica e dinamica quaternaria (Testo stamp.) 45 (1), pp. 19–40

DOI: 10.4461/ GFDQ.2022.45.2

2022, Dataset, ENG

Rock temperature variability in the alpine cryosphere

Nigrelli G., Chiarle M., Merlone A., Coppa G., Musacchio C.

In a context of cryosphere degradation caused by climate warming, rock temperature is one of the main driving factors of rockfalls that occur on high-elevation mountain slopes. In order to improve the knowledge of this critical relationship, it is necessary to increase measurement capability of rock temperature and its variability in different lithological and slope/aspect conditions, and also to increase local scale studies, increasing the quality and the comparability of the data. Rock temperature data, acquired from July 2018 to July 2022 in an alpine experimental glacial basin (https://deims.org/f8718e56-fb4d-49a3-92a9-3670e7f10ee9), in different two temperature monitoring sites (TMS) with the same lithological conditions (calc-schists) but in two different aspect conditions (South and North), at an elevation range from 2653 to 2667 m a.s.l, are present. The temperature data have been acquired by using six MadgeTech MicroTemp Data Logger (MT), metrologically referenced and with known measurement uncertainty (0.098 °C).

2022, Articolo in rivista, ENG

Co-design of sectoral climate services based on seasonal prediction information in the Mediterranean

Sanchez-Garcia E.; Rodriguez-Camino E.; Bacciu V.; Chiarle M.; Costa-Saura J.; Garrido M.N.; Lledo L.; Navascues B.; Paranunzio R.; Terzago S.; Bongiovanni G.; Mereu V.; Nigrelli G.; Santini M.; Soret A.; von Hardenberg J.

We present in this contribution the varied experiences gathered in the co-design of a sectoral climate services collection, developed in the framework of the MEDSCOPE project, which have in common the application of seasonal predictions for the Mediterranean geographical and climatic region. Although the region is affected by low seasonal predictability limiting the skill of seasonal forecasting systems, which historically has hindered the development of downstream services, the project was originally conceived to exploit windows of opportunity with enhanced skill for developing and evaluating climate services in various sectors with high societal impact in the region: renewable energy, hydrology, and agriculture and forestry. The project also served as the scientific branch of the WMO-led Mediterranean Climate Outlook Forum (MedCOF) that had as objective -among others- partnership strengthening on climate services between providers and users within the Mediterranean region. The diversity of the MEDSCOPE experiences in co-designing shows the wide range of involvement and engagement of users in this process across the Mediterranean region, which benefits from the existing solid and organized MedCOF community of climate services providers and users. A common issue among the services described here -and also among other prototypes developed in the project- was related with the communication of forecasts uncertainty and skill for efficiently informing decision-making in practice. All MEDSCOPE project prototypes make use of an internally developed software package containing process-based methods for synthesising seasonal forecast data, as well as basic and advanced tools for obtaining tailored products. Another challenge assumed by the project refers to the demonstration of the economic, social, and environmental value of predictions provided by these MEDSCOPE prototypes.

Climate services 28

DOI: 10.1016/j.cliser.2022.100337

2022, Abstract in rivista, ENG

Co-design of sectoral climate services based on seasonal prediction information in theMediterranean

Esteban Rodríguez-Guisado (1), Ernesto Rodríguez-Camino (1), Eroteida Sánchez-García (2), Valentina Bacciu (3), Marta Chiarle (4), Jose Costa-Saura (3), Maria Nieves Garrido (5), Llorenç Lledo6, Beatriz Navascués (1), Roberta Paranunzio (4), Silvia Terzago (4), Valentina Mereu (3), Guido Nigrelli (4), Monia Santini (3), Albert Soret (6), and Jost von Hardenberg (4)

We present in this contribution the varied experiences gathered in the co-design of a sectoral climate services collection, developed in the frame of the MEDSCOPE project. This colletion of climate services have in common the application of seasonal predictions for the Mediterranean geographical and climatic region. The project was originally conceived to develop and evaluate climate services for various sectors with high societal impact in the region: renewable energy, hydrology, and agriculture and forestry. The project also served as the scientific branch of the WMO led Mediterranean Climate Outlook Forum (MedCOF) that had as objective -among others- partnership strengthening on climate services between providers and users within the Mediterranean region. The diversity of the MEDSCOPE experiences in co-designing shows the wide range of involvement and engagement of users in this process across the Mediterranean region, which benefits from an existing solid and organized community of climate services providers and users. A common issue among the services described here -and also among other prototypes developed in the project- was related with the communication of forecasts uncertainty and skill for efficiently informing decision-making in practice. Another challenge concerns the demonstration of the economic, social, and environmental value of predictions provided by these MEDSCOPE prototypes.

EMS Annual Meeting Abstracts 19 (EMS2022-667)

2022, Presentazione, ENG

Rock temperature measurements in high-alpine cryosphere: the role of metrology

G. Coppa, G. Nigrelli, M. Chiarle, A. Merlone, C. Musacchio

no abstract

5th Arctic Metrology Workshop, Longyearbyen, Svalbard, Norway, 8-9 June 2022

2022, Presentazione, ENG

Potentialities of Sentinel-2 images for the study of the fresh water resource in a mountainous catchment

Matta Erica1, Giardino Claudia1, Bresciani Mariano1, Chiarle Marta2, Nigrelli Guido2

Water quality and availability are nowadays essential requirements for all those activities that need an exploitation of the water resource: e.g. potable use, hydroelectricity production, agriculture, recreation. Inland water originates from atmospheric events and is stored in solid state as glaciers or snow (e.g. on the mountains) or in natural and artificial lakes at any altitude. The well documented climate warming has, among its multiple effects, the modification of the equilibrium between liquid and solid phase of water, its storage and availability, as well as changes in the precipitation regime, such as the reduction and intensification of rainfall events alternated to long aridity periods. All these changes alter water quality and water availability at catchment level. We are experimenting the use of earth observation data (Sentinel-2) to track temporal variations of land covers, lake surface and lake water colour over the last 5 years in a small high-altitude catchment in Italy (e.g. Lake Ceresole watershed, Orco Valley, Piedmont). Here, satellite derived data (e.g. snow cover and water colour), coupled with available meteorological data (e.g. precipitation), are analysed in order to find possible correlations between water colour and snow melting, or water colour changes following strong or extreme meteorological events. Water colour is a largely recognised proxy of water quality. In particular, in mountainous environments, where the anthropic pressure is minimized and natural processes are prevailing, water colour is mainly driven by the presence of solid sediments inside the water. These sediments can be released due to the melting of snow and ice, particularly during thaw periods, thus at seasonal timescale, with possible variations among different years (these variations due to particular meteorological conditions relative to each single year). Also, solid transport as river flow or runoff, can be generated as a consequence of heavy rainfall events, and those sediments can reach the lakes within the catchment modifying their water colour. With this study, we would like to understand if the high spatial resolution of Sentinel-2 acquisitions (i.e. 10m) and its revisit time (2-5 days), except for the drawbacks of all optical satellite sensors (e.g. cloud cover), can provide useful information to follow the on-going modifications that the mountainous environment is facing due to the global warming. The use of earth observation data for this purpose would be a valuable tool in helping both monitoring and understanding of climate change consequences, and in managing the water resource in places not easily accessible for periodic in-situ measures. In fact, mountains represent both the ideal location where nature responds to climatic pressures, but also, they constitute the water sink of fresh water for downstream valleys.

EGU 2022, Vienna, Austria, 23/05/2022, 27/05/2022

2022, Contributo in volume, ITA

Temperature in aumento nell'ambiente periglaciale alpino

Nigrelli G., Chiarle M.

Sulle Alpi europee, negli ultimi decenni, la temperatura dell'aria mostra un riscaldamento a un tasso medio di 0,3 °C/10 anni, un valore superiore al tasso di riscaldamento globale che è di 0,2 °C/10 anni. L'ambiente periglaciale alpino è particolarmente importante per diversi aspetti (es. energetico, ecologico e turistico). Tuttavia mancano studi specifici e aggiornati relativi alle tendenze della temperatura in questo ambiente. Per colmare questa lacuna sono state analizzate le tendenze delle temperature per il periodo 1990-2019. L'ambiente periglaciale delle Alpi ha mostrato un tasso di riscaldamento di 0,4 °C/10 anni, 0,6 °C/10 anni e 0,8 °C/10 anni rispettivamente per la temperatura media, massima e minima. Questi tassi di riscaldamento sono superiori a quelli osservati per l'intera area alpina. Nel 2050 si prevede l'estinzione di molti ghiacciai delle Alpi al di sotto dei 3000 m di altitudine e tutte le aree precedentemente occupate dai ghiacciai diventeranno periglaciali.

2022, Articolo in rivista, ENG

Rock temperature variability in high-altitude rockfall-prone areas

Nigrelli G., Chiarle M., Merlone A., Coppa G., Musacchio C.

In a context of cryosphere degradation caused by climate warming, rock temperature is one of the main driving factors of rockfalls that occur on high-elevation mountain slopes. In order to improve the knowledge of this critical relationship, it is necessary to increase measurement capability of rock temperature and its variability in different lithological and slope/aspect conditions, and also to increase local scale studies, increasing the quality and the comparability of the data. This paper shows an example of metrological characterization of sensors used for rock temperature measurement in mountain regions, by means of the measurement uncertainty. Under such approach, data and results from temperature measurements carried out in the Bessanese high-elevation experimental site (Western European Alps) are illustrated. The procedures for the calibration and field characterization of sensors allow to measure temperature in different locations, depths and lithotypes, within 0.10 °C of overall uncertainty. This work has highlighted that metrological traceability is fundamental to asses data quality and establish comparability among different measurements; that there are strong differences between air temperature and near-surface rock temperature; and that there are significant differences of rock temperature acquired in different aspect conditions. Finally, solar radiation, slope/aspect conditions and lithotype, seem to be the main driving factors of rock temperature.

Journal of mountain science (Online) 19 (3), pp. 798–811

DOI: 10.1007/s11629-021-7073-z

2022, Contributo in volume, ENG

Assessment Principles for Glacier and Permafrost Hazards in Mountain Regions

Allen, S. (1, 2), Frey, H. (1), Haeberli, W. (1), Huggel, C. (1), Chiarle, M. (3), & Geertsema, M. (4)

Glacier and permafrost hazards in cold mountain regions encompass various flood and mass movement processes that are strongly affected by rapid and cumulative climate-induced changes in the alpine cryosphere. These processes are characterized by a range of spatial and temporal dimensions, from small volume icefalls and rockfalls that present a frequent but localized danger to less frequent but large magnitude process chains that can threaten people and infrastructure located far downstream. Glacial lake outburst floods (GLOFs) have proven particularly devastating, accounting for the most far-reaching disasters in high mountain regions globally

DOI: 10.1093/acrefore/9780199389407.013.356

2022, Altro prodotto, ITA

Aumento delle temperature: l'impatto ambientale sulle Alpi

Guido Nigrelli, Marta Chiarle

le temperature aumentano in modo evidente un po' dappertutto. L'Intergovernmental Panel on Climate Change (IPCC), uno dei più autorevoli organismi internazionali in tema di cambiamenti climatici, afferma che negli ultimi decenni il tasso di riscaldamento sulle Alpi è stato di 0,3 °C/10 anni, superando il tasso di riscaldamento globale che è stato di 0,2 °C/10 anni. In uno studio recentemente concluso dimostriamo come, sulle Alpi, l'ambiente periglaciale presenta tassi di riscaldamento maggiori rispetto a quelli dell'intera area alpina.

2021, Articolo in rivista, ITA

Frane di alta quota: Sentinelle dei cambiamenti climatici

Marta Chiarle

High mountains are the realm of the cryosphere: snow, glaciers and permafrost give charm to mountain slopes, but at the same time protect them from atmospheric agents and contribute to their stability. Climate change, and in particular temperature increase, is however causing cryosphere reduction, exposing high mountains to an increasing instability. In this context, landslides are both an effect and an indicator of climate change impact on terrestrial systems. In particular from the hot summer of 2003, awareness of the ongoing climate change and its effects has gradually grown, thanks also to international research efforts. An alliance between citizens, public administrations and research institutions is urgently needed to understand the ongoing changes, develop future scenarios, and tackle climate change and its impacts.

Notiziario della Banca Popolare di Sondrio 146, pp. 32–37

2021, Articolo in rivista, ENG

Evolution of temperature indices in the periglacial environment of the European Alps in the period 1990-2019

Nigrelli G., Chiarle M.

Air temperature in the European Alps shows warming over recent decades at an average rate of 0.3 °C/10 years, thereby outpacing the global warming rate of 0.2 °C/10 years. The periglacial environment of the Alps is particularly important for several aspects (i.e. hydropower production, tourism, natural hazards, indicator of global warming). However, there is a lack of specific and updated studies relating to temperature change in this environment. In order to fill this gap, the recent temperature trends in the periglacial environment of the Alps were analyzed. Mean/maximum/minimum daily air temperatures recorded by 14 land-based meteorological stations were used, and the temperature indices for the period 1990-2019 were calculated. The periglacial environment of the Alps showed a warming rate of 0.4 °C/10 years, 0.6 °C/10 years and 0.8 °C/10 years for the mean/maximum/minimum temperatures, respectively. These warming rates are higher than that observed for the entire Alpine area. In 2050 many glaciers of the Alps below 3000 m altitude are expected to be extinct, and all the areas previously occupied by glaciers will become periglacial. In order to manage and adapt to these changes, more in-depth climate analyses are needed. This is necessary for all the mountainous areas of the world, which are undergoing similar changes.

Journal of mountain science (Online) 18 (11), pp. 2842–2853

DOI: 10.1007/s11629-021-6889-x

InstituteSelected 0/8
    IRPI, Istituto di ricerca per la protezione idrogeologica (220)
    IGG, Istituto di geoscienze e georisorse (13)
    ISAC, Istituto di scienze dell'atmosfera e del clima (6)
    IGAG, Istituto di geologia ambientale e geoingegneria (1)
    IMAMOTER, Istituto per le macchine agricole e movimento terra (1)
    ISEM, Istituto di storia dell'Europa mediterranea (1)
    ISMAR, Istituto di scienze marine (1)
    ISTI, Istituto di scienza e tecnologie dell'informazione "Alessandro Faedo" (1)
AuthorSelected 1/12016

Chiarle Marta

    Drioli Enrico (1623)
    Pasetto Gaia (1193)
    Passer Mauro (1184)
    Arico' Antonino Salvatore (983)
    Ambrosio Luigi (981)
    Di Marzo Vincenzo (976)
    Ferrari Maurizio (948)
    Viegi Giovanni (906)
    Antonucci Vincenzo (866)
    Ferraro Pietro (849)
TypeSelected 0/19
    Articolo in rivista (63)
    Contributo in atti di convegno (39)
    Poster (26)
    Contributo in volume (25)
    Presentazione (20)
    Abstract in atti di convegno (18)
    Banca dati (11)
    Abstract in rivista (8)
    Rapporto di ricerca (Research report) (7)
    Altro prodotto (6)
Research programSelected 0/25
    TA.P05.006.016, Ruolo dei cambiamenti climatici nella morfogenesi dell'ambiente glaciale-periglaciale e analisi dei rischi associati (97)
    DTA.AD003.104.001, Ruolo dei cambiamenti climatici nella morfogenesi dell'ambiente glaciale-periglaciale e analisi dei rischi associati (35)
    DTA.AD003.208.001, RiST2 la ricerca continua (14)
    TA.P02.011.002, Evoluzione recente ed attuale dell'ambiente glaciale e periglaciale e analisi di serie temporali di dati idrologici (9)
    TA.P05.006.002, Valutazione del rischio posto da fenomeni geo-idrologici e sviluppo di strategie di mitigazione (9)
    DTA.AD003.718.001, GLARIS-SP (6)
    DTA.AD003.547.001, GioMon (5)
    TA.P05.005.002, Frane e altri movimenti in massa: cause, dinamiche ed effetti sull’ambiente (5)
    TA.P05.006.014, Rischio geo-idrologico in ambiente alpino (5)
    TA.P05.010.001, Tecniche e tecnologie per il monitoraggio dei parametri che caratterizzano le evoluzioni morfologiche di alvei e versanti instabili. (5)
EU Funding ProgramSelected 0/1
    H2020 (1)
EU ProjectSelected 0/1
    HYPOS (1)
YearSelected 0/28
    2014 (22)
    2017 (20)
    2013 (18)
    2009 (15)
    2011 (15)
    2007 (13)
    2015 (12)
    2019 (12)
    2021 (11)
    2022 (11)
LanguageSelected 0/3
    Inglese (136)
    Italiano (83)
    Francese (4)
KeywordSelected 0/286
    Italian Alps (16)
    Climate change (14)
    Alpi (12)
    Alps (12)
    alpi (12)
    Temperature (9)
    climate change (8)
    Glaciers (7)
    cryosphere (7)
    ghiacciai (7)
RESULTS FROM 1 TO 20 OF 243