Nocturnal convection initiation accounts for nearly half of all CI events (daytime and nighttime) over the Great Plains over the warm season. There are three main types of CI events: those that occur on surface boundaries, those that occur on the cold side of surface boundaries, and those that occur with no nearby surface boundaries (NB [no boundary] CI mode). This study focuses on the poorly-understood NB nocturnal CI mode events. These storms typically occur in environments with weak forcing or occur far away from preexisting convection and away from surface boundaries. There are preferred characteristics to these events, however. For example, these events form later at night (around 0900 UTC), occur on the eastern side of the low-level j...
There has been a recent wave of attention given to atmospheric bores in order to understand how they...
Nighttime convective storms produce a significant portion of warm season precipitation across the Gr...
<p>This study examines whether and how land-atmosphere interactions can have an impact on the noctur...
A remarkable feature of the regional climatology of the central United States and the Great Plains i...
Nocturnal convection is a common feature of the Great Plains region. Forecasting this convection, ho...
A nocturnal maximum in precipitation exists over the Great Plains during the summer. The initiation ...
Accurate representation of bores in forecast models is a challenge. This challenge is of considerab...
A new mechanism is proposed as a potential cause for the one-third of warm season severe nocturnal c...
The prediction of convective initiation remains a challenge to forecasters in the Great Plains, espe...
The central Great Plains region in North America has a nocturnal maximum in warm-season precipitatio...
Most continental regions experience an afternoon or evening maximum of convective activity, which is...
There has been a recent wave of attention given to atmospheric bores in order to understand how they...
Numerical weather prediction (NWP) models often fail to correctly forecast both the initiation and e...
The nocturnal low-level jet (NLLJ) is a maximum in the vertical wind profile often occurring in the ...
Although nocturnal convection is frequently observed, the mechanisms that allow nocturnal mesoscale ...
There has been a recent wave of attention given to atmospheric bores in order to understand how they...
Nighttime convective storms produce a significant portion of warm season precipitation across the Gr...
<p>This study examines whether and how land-atmosphere interactions can have an impact on the noctur...
A remarkable feature of the regional climatology of the central United States and the Great Plains i...
Nocturnal convection is a common feature of the Great Plains region. Forecasting this convection, ho...
A nocturnal maximum in precipitation exists over the Great Plains during the summer. The initiation ...
Accurate representation of bores in forecast models is a challenge. This challenge is of considerab...
A new mechanism is proposed as a potential cause for the one-third of warm season severe nocturnal c...
The prediction of convective initiation remains a challenge to forecasters in the Great Plains, espe...
The central Great Plains region in North America has a nocturnal maximum in warm-season precipitatio...
Most continental regions experience an afternoon or evening maximum of convective activity, which is...
There has been a recent wave of attention given to atmospheric bores in order to understand how they...
Numerical weather prediction (NWP) models often fail to correctly forecast both the initiation and e...
The nocturnal low-level jet (NLLJ) is a maximum in the vertical wind profile often occurring in the ...
Although nocturnal convection is frequently observed, the mechanisms that allow nocturnal mesoscale ...
There has been a recent wave of attention given to atmospheric bores in order to understand how they...
Nighttime convective storms produce a significant portion of warm season precipitation across the Gr...
<p>This study examines whether and how land-atmosphere interactions can have an impact on the noctur...