During the International H2O Project (IHOP) in the Southern U.S. Central Plains in May and June 2002, aircraft missions on June 3 and June 9 2002 made detailed lidar and dropsonde observations of intense phases of the low-level jet (LLJ) . Combined with standard and enhanced operational observations (primarily radiosondes and profilers) and other ground-based research observations, data from these missions represent an unprecedented opportunity to describe moisture transport in the LLJ at scales ranging from the synoptic scales resolved by the radiosonde network to sub-mesoscale features in the moisture and wind fields observed by airborne lidar instruments
The classic Great Plains southerly low-level jet (LLJ) is a primary factor in sustaining nocturnal c...
The nocturnal low-level jet (NLLJ) is a maximum in the vertical wind profile often occurring in the ...
This study presents a comprehensive analysis of the variability of water vapour in a growing convect...
Previous studies of the Low-Level Jet (LLJ) over the Central Great Plains of the U.S. have been unab...
Low-level jets (LLJs) can be defined as wind corridors of anomalously high wind speed values located...
Moisture transported by the low level jet (LLJ) from the Gulf of Mexico into the Central Great Plain...
A unique dataset obtained with combinations of minisodars and 915-MHz wind profilers at the Atmosphe...
dissertationThe synoptic and mesoscale connections between Low-Level Jets (LLJ) and precipitation in...
Two cases of low-level jet (LLJ) support the hypothesis that the LLJ is an integral part of synoptic...
The keynote talk summarized five years of work simulating observed mesoscale convective systems with...
Low-level-jet (LLJ) periods are investigated by exploiting a long-termrecord of ground-based remote ...
International audienceThis study presents a comprehensive analysis of the variability of water vapou...
Water vapor, a minor constituent of the earth’s atmosphere, plays a major role in the radiation budg...
The Great Plains low-level jet (LLJ) fosters an environment that supports nocturnal mesoscale convec...
The first collocated measurements during THORPEX (The Observing System Research and Predictability ...
The classic Great Plains southerly low-level jet (LLJ) is a primary factor in sustaining nocturnal c...
The nocturnal low-level jet (NLLJ) is a maximum in the vertical wind profile often occurring in the ...
This study presents a comprehensive analysis of the variability of water vapour in a growing convect...
Previous studies of the Low-Level Jet (LLJ) over the Central Great Plains of the U.S. have been unab...
Low-level jets (LLJs) can be defined as wind corridors of anomalously high wind speed values located...
Moisture transported by the low level jet (LLJ) from the Gulf of Mexico into the Central Great Plain...
A unique dataset obtained with combinations of minisodars and 915-MHz wind profilers at the Atmosphe...
dissertationThe synoptic and mesoscale connections between Low-Level Jets (LLJ) and precipitation in...
Two cases of low-level jet (LLJ) support the hypothesis that the LLJ is an integral part of synoptic...
The keynote talk summarized five years of work simulating observed mesoscale convective systems with...
Low-level-jet (LLJ) periods are investigated by exploiting a long-termrecord of ground-based remote ...
International audienceThis study presents a comprehensive analysis of the variability of water vapou...
Water vapor, a minor constituent of the earth’s atmosphere, plays a major role in the radiation budg...
The Great Plains low-level jet (LLJ) fosters an environment that supports nocturnal mesoscale convec...
The first collocated measurements during THORPEX (The Observing System Research and Predictability ...
The classic Great Plains southerly low-level jet (LLJ) is a primary factor in sustaining nocturnal c...
The nocturnal low-level jet (NLLJ) is a maximum in the vertical wind profile often occurring in the ...
This study presents a comprehensive analysis of the variability of water vapour in a growing convect...