Snow cover estimation is a principal source of error for spring streamflow simulations in Québec, Canada. Optical and near infrared remote sensing can improve snow cover area (SCA) estimation due to high spatial resolution but is limited by cloud cover and incoming solar radiation. Passive microwave remote sensing is complementary by its near-transparence to cloud cover and independence to incoming solar radiation, but is limited by its coarse spatial resolution. The study aims to create an improved SCA product from blended passive microwave (AMSR-E daily L3 Brightness Temperature) and optical (MODIS Terra and Aqua daily snow cover L3) remote sensing data in order to improve estimation of river streamflow caused by snowmelt with Québec's op...
Soil moisture (SM) plays a key role in meteorology, hydrology, and ecology as it controls the evolut...
Snow cover estimation is a principal source of error for spring streamflow simulations in Québec, Ca...
The use of weather radar data to estimate rainfall accumulations is often complicated by the heighto...
The Centre d'expertise hydrique du Québec (CEHQ) operates a distributed hydrological model (MOHYSE),...
The spatial/temporal variation of the snow cover is simulated by many models such as the Canadian Re...
An accurate seasonal snowpack modeling is needed to study its evolution and to improvethe avalanche ...
The cryosphere has a key role in the climate system, among others because it reflects a significant ...
Une modélisation précise du manteau neigeux saisonnier est indispensable pour comprendre son évoluti...
Une estimation précise de l'évapotranspiration (ET) à grand échelle est une priorité pour comprendre...
Accurate understanding of the land surface functioning, such as the energy budget, carbon and water ...
Monitoring and representing the snowpack variability in mountains are crucial ecological and societa...
SMOS and SMAP passive microwave sensors provide soil moisture (SM) data at 40 km resolution every 2-...
The current generation of advanced infrared sounders is one of the most important sources of observa...
Soil freezing and thawing processes are of particular importance for agricultural areas. For example...
Soil moisture (SM) plays a key role in meteorology, hydrology, and ecology as it controls the evolut...
Snow cover estimation is a principal source of error for spring streamflow simulations in Québec, Ca...
The use of weather radar data to estimate rainfall accumulations is often complicated by the heighto...
The Centre d'expertise hydrique du Québec (CEHQ) operates a distributed hydrological model (MOHYSE),...
The spatial/temporal variation of the snow cover is simulated by many models such as the Canadian Re...
An accurate seasonal snowpack modeling is needed to study its evolution and to improvethe avalanche ...
The cryosphere has a key role in the climate system, among others because it reflects a significant ...
Une modélisation précise du manteau neigeux saisonnier est indispensable pour comprendre son évoluti...
Une estimation précise de l'évapotranspiration (ET) à grand échelle est une priorité pour comprendre...
Accurate understanding of the land surface functioning, such as the energy budget, carbon and water ...
Monitoring and representing the snowpack variability in mountains are crucial ecological and societa...
SMOS and SMAP passive microwave sensors provide soil moisture (SM) data at 40 km resolution every 2-...
The current generation of advanced infrared sounders is one of the most important sources of observa...
Soil freezing and thawing processes are of particular importance for agricultural areas. For example...
Soil moisture (SM) plays a key role in meteorology, hydrology, and ecology as it controls the evolut...
Snow cover estimation is a principal source of error for spring streamflow simulations in Québec, Ca...
The use of weather radar data to estimate rainfall accumulations is often complicated by the heighto...