André Bertoncini

ORCID: 0000-0003-4663-2858
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About
Contact & Profiles
Research Areas
  • Cryospheric studies and observations
  • Meteorological Phenomena and Simulations
  • Flood Risk Assessment and Management
  • Precipitation Measurement and Analysis
  • Climate change and permafrost
  • Hydrology and Watershed Management Studies
  • Climate variability and models
  • Fire effects on ecosystems
  • Soil erosion and sediment transport
  • Arctic and Antarctic ice dynamics
  • Atmospheric and Environmental Gas Dynamics
  • Landslides and related hazards
  • Geophysics and Gravity Measurements
  • 3D Surveying and Cultural Heritage
  • Soil Moisture and Remote Sensing
  • Clinical Nutrition and Gastroenterology
  • 3D Modeling in Geospatial Applications
  • Methane Hydrates and Related Phenomena
  • Atmospheric aerosols and clouds
  • Ionosphere and magnetosphere dynamics
  • Healthcare Systems and Challenges
  • Tropical and Extratropical Cyclones Research
  • Tree-ring climate responses
  • Geology and Paleoclimatology Research

University of Saskatchewan
2019-2025

Canmore Museum and Geoscience Centre
2022-2024

National Institute for Space Research
2016-2019

Abstract Wildfire occurrence and severity is predicted to increase in the upcoming decades with severe negative impacts on human societies. The of upwind wildfire activity glacier melt, a critical source freshwater for downstream environments, were investigated through analysis field remote sensing observations modeling experiments 2015–2020 melt seasons at well‐instrumented Athabasca Glacier Canadian Rockies. Upwind influenced surface both decrease albedo from deposition soot impact smoke...

10.1029/2022ef002685 article EN Earth s Future 2022-04-01

Abstract. Uncertainty in estimating precipitation mountain headwaters can be transmitted to estimates of river discharge far downstream. Quantifying and reducing this uncertainty is needed better constrain the hydrological predictions rivers with headwaters. Spatial estimation fields accomplished through interpolation snowfall rainfall observations. These are often sparse mountains, so gauge density greatly affects uncertainty. Elevational lapse rates also influence as they vary widely...

10.5194/hess-29-983-2025 article EN cc-by Hydrology and earth system sciences 2025-02-25

Abstract Reliable precipitation forcing is essential for calculating the water balance and other hydrological variables. However, satellite often only available to run models in data‐scarce regions compromising calculations. The Integrated Multi‐satellitE Retrievals GPM (IMERG) product estimates from passive microwave infrared satellites, which are intercalibrated based on Global Precipitation Measurement (GPM)'s Dual‐frequency Radar (DPR) Microwave Image (GMI) instruments. GPM‐DPR radar...

10.1029/2024jd041481 article EN cc-by-nc Journal of Geophysical Research Atmospheres 2025-03-03

Abstract The Canadian Rockies are a triple-continental divide, whose high mountains drained by major snow-fed and rain-fed rivers flowing to the Pacific, Atlantic, Arctic Oceans. objective of April–June 2019 Storms Precipitation Across continental Divide Experiment (SPADE) was determine atmospheric processes producing precipitation on eastern western sides during springtime, period when upslope events variable phase dominate slopes. To do so, three observing sites across divide were...

10.1175/bams-d-21-0146.1 article EN Bulletin of the American Meteorological Society 2022-09-14

Abstract. The continental divide along the spine of Canadian Rockies in southwestern Canada is a critical headwater region for hydrological drainages to Pacific, Arctic, and Atlantic oceans. Major flooding events are typically attributed heavy precipitation on its eastern side due upslope (easterly) flows. Precipitation can also occur western when moisture originating from Pacific Ocean encounters west-facing slopes Rockies. Often, storms propagating across result significant both sides....

10.5194/essd-13-1233-2021 article EN cc-by Earth system science data 2021-03-24

This paper provides an early career researchers (ECRs) perspective on major challenges and opportunities that arise in the study understanding of, provision of regional information for Climate, Weather Hydrological (CWH) extreme events. emerged from discussions three-day Young Earth System Scientists - Hydrologic Society (YESS-YHS) workshop, which was conjointly held with Global Energy Water Exchanges (GEWEX) Open Science Conference. In this we discuss three possible ways forward field: a...

10.3389/fenvs.2019.00006 article EN cc-by Frontiers in Environmental Science 2019-02-04

Wildfires and heatwaves have recently affected the hydrological system in unprecedented ways due to climate change. In cold regions, these extremes cause rapid reductions snow ice albedo soot deposition unseasonal melt. Snow dynamics control net shortwave radiation available energy for melt runoff generation. Many algorithms models cannot accurately simulate because they were developed or parameterised based on historical observations. Remotely sensed data assimilation (DA) can potentially...

10.22541/au.171128344.49725407/v1 preprint EN Authorea (Authorea) 2024-03-24

Abstract. Uncertainty in estimating precipitation mountain headwaters can be transmitted to estimates of river discharge far downstream. Quantifying and reducing this uncertainty is needed better constrain the hydrological predictions rivers with headwaters. Spatial estimation fields accomplished through interpolation snowfall rainfall observations, these are often sparse mountains so gauge density strongly affects uncertainty. Elevational lapse rates also influence as they vary widely...

10.5194/egusphere-2024-288 preprint EN cc-by 2024-02-02

Reliable precipitation forcing is essential for calculating the water balance, seasonal snowpack, glacier mass streamflow, and other hydrological variables. However, satellite often only available to run models in data-scarce regions, compromising calculations when unreliable. The IMERG product estimates quasi-globally from a combination of passive microwave infrared satellites, which are intercalibrated based on GPM’s DPR GMI instruments. Current GPM-DPR radar algorithms have satisfactorily...

10.22541/essoar.171535990.06146530/v1 preprint EN Authorea (Authorea) 2024-05-10

ABSTRACT Wildfires and heatwaves have recently affected the hydrological system in unprecedented ways due to climate change. In cold regions, these extremes cause rapid reductions snow ice albedo soot deposition unseasonal melt. Snow dynamics control net shortwave radiation available energy for melt runoff generation. Many algorithms models cannot accurately simulate because they were developed or parameterised based on historical observations. Remotely sensed data assimilation (DA) can...

10.1002/hyp.15329 article EN Hydrological Processes 2024-11-01

O presente trabalho apresenta uma proposta metodológica para avaliar o potencial adicional de construção urbana apartir dados LiDAR e uso parametrização objetos tridimensionais. objetivo da pesquisa foi quantificar ovalor do espaço não construído com fins lançamento CEPAC (Certificados PotencialAdicional Construção), a partir modelagem software CityEngine utilização aéreos deperfilamento laser (LiDAR). A área estudo está localizada em Joinville-SC, onde foram recolhidos os eos parâmetros...

10.14393/rbcv67n0-49231 article PT cc-by-nc Revista Brasileira de Cartografia 2019-06-17

Hydrological modelling is largely applied to forecast the effects of extreme rainfall on runoff dynamics. Little research has been done coupling numerical weather prediction (NWP) and hydrological in southern Brazil given limited hydrometeorological NWP data available for region. In this study, we evaluate a method semi-distributed model humid subtropical catchment (286 km²) Brazil, state Santa Catarina, municipality Vidal Ramos. The HEC-HMS was manually calibrated validated using 2013. Four...

10.5935/rbgf.v9i6.1812 article EN Revista Brasileira de Geografia Física 2016-10-31

Hydrological modelling is largely applied to forecast the effects of extreme rainfall on runoff dynamics. Little research has been done coupling numerical weather prediction (NWP) and hydrological in southern Brazil given limited hydrometeorological NWP data available for region. In this study, we evaluate a method semi-distributed model humid subtropical catchment (286 km²) Brazil, state Santa Catarina, municipality Vidal Ramos. The HEC-HMS was manually calibrated validated using 2013. Four...

10.26848/rbgf.v9.6.p1990-2002 article EN cc-by Revista Brasileira de Geografia Física 2016-10-31

Global Water Future’s Storms and Precipitation Across the continental Divide Experiment (SPADE) was initiated to enhance our knowledge of contribution different moisture flows on precipitation across Canadian Rockies. SPADE installed instrumentation both sides divide gather automated manual observations during an intensive field campaign from 24 April 26 June 2019. Various meteorological instruments were deployed including a two Doppler LiDARs, three vertically pointing micro rain radars...

10.20383/101.0221 article EN 2020-05-11

Abstract. The continental divide along the spine of Canadian Rockies in southwestern Canada is a critical headwater region for hydrological drainages to Pacific, Arctic, and Atlantic oceans. Major flooding events are typically attributed heavy precipitation on its eastern side due upslope (easterly) flows. Precipitation can also occur western when moisture originating from Pacific Ocean encounters west-facing slopes Rockies. In other storms, substantial fall both sides. Meteorological data...

10.5194/essd-2020-160 preprint EN cc-by 2020-10-17
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