Improving process-based prediction of stream water temperature in SWAT using semi-Lagrangian formulation
ND Melaku, CW Brown, AA Tavakoly - Journal of Hydrology, 2025 - Elsevier
Accurately predicting stream water temperature at large scales requires modeling
techniques that account for various physical, chemical, and biological processes that …
techniques that account for various physical, chemical, and biological processes that …
Effect of urban heat island mitigation strategies on precipitation and temperature in Montreal, Canada: Case studies
High-resolution numerical weather prediction experiments using the Global Environmental
Multiscale (GEM) model at a 250-m horizontal resolution are used to investigate the effect of …
Multiscale (GEM) model at a 250-m horizontal resolution are used to investigate the effect of …
Incorporating physically-based water temperature predictions into the National water model framework
While river water temperatures are a strong control on instream processes and aquatic
ecosystems, monitoring networks for river water temperatures are often sparse. Despite …
ecosystems, monitoring networks for river water temperatures are often sparse. Despite …
[HTML][HTML] A new dynamical core of the Global Environmental Multiscale (GEM) model with a height-based terrain-following vertical coordinate
SZ Husain, C Girard, A Qaddouri… - Monthly Weather …, 2019 - journals.ametsoc.org
Caya, A., R. Laprise, and P. Zwack, 1998: Consequences of using the splitting method for
implementing physical forcings in a semi-implicit semi-Lagrangian model. Mon. Wea. Rev …
implementing physical forcings in a semi-implicit semi-Lagrangian model. Mon. Wea. Rev …
Convectively transported water vapor plumes in the midlatitude lower stratosphere
Deep convective overshooting has been shown to transport water vapor into the midlatitude
lower stratosphere. However, it has not been demonstrated how the convective water vapor …
lower stratosphere. However, it has not been demonstrated how the convective water vapor …
A convection parameterization for low-CAPE environments
R McTaggart-Cowan, PA Vaillancourt… - Monthly Weather …, 2020 - journals.ametsoc.org
Numerical models that are unable to resolve moist convection in the atmosphere employ
physical parameterizations to represent the effects of the associated processes on the …
physical parameterizations to represent the effects of the associated processes on the …
Sweep interpolation: a cost-effective semi-Lagrangian scheme in the Global Environmental Multiscale model
The interpolation process is the most computationally expensive step of the semi-
Lagrangian (SL) approach for solving advection and is commonly used in numerical …
Lagrangian (SL) approach for solving advection and is commonly used in numerical …
IMERG in the Canadian Precipitation Analysis (CaPA) System for Winter Applications
S Bélair, PN Feng, F Lespinas, D Khedhaouiria… - Atmosphere, 2024 - mdpi.com
Several configurations of the Canadian Precipitation Analysis system (CaPA) currently
produce precipitation analyses at Environment and Climate Change Canada (ECCC). To …
produce precipitation analyses at Environment and Climate Change Canada (ECCC). To …
[HTML][HTML] Physical and Statistical Links between Errors at the Surface, in the Boundary Layer, and in the Free Atmosphere in Medium-Range Numerical Weather …
The adequate representation of interactions between the land surface and the atmosphere
is of crucial importance in modern numerical weather prediction (NWP) systems. In this …
is of crucial importance in modern numerical weather prediction (NWP) systems. In this …
A fast converging and concise algorithm for computing the departure points in semi‐Lagrangian weather and climate models
M Diamantakis, F Váňa - Quarterly Journal of the Royal …, 2022 - Wiley Online Library
Accurate calculation of departure points is crucial for the overall accuracy of a semi‐
Lagrangian advection scheme. The iterative method used in the semi‐Lagrangian advection …
Lagrangian advection scheme. The iterative method used in the semi‐Lagrangian advection …