| Call Number (LC) | Title | Results |
|---|---|---|
| QC880.4 .B65 O27 2002 | Observation of the atmospheric boundary layer in the western and central Gulf of Mexico final performance report / | 1 |
| QC880.4 .B65 O274 2000 | Observation of the atmospheric boundary layer in the western and central Gulf of Mexico second annual report / | 1 |
| QC880.4.B65 O36 1984 | Boundary Layer Structure : Modeling and Application to Air Pollution and Wind Energy / | 1 |
| QC880.4.B65 S67 1989 | Structure of the atmospheric boundary layer / | 1 |
| QC880.4.B65 S73 1994 | Stably stratified flows : flow and dispersion over topography : based on the proceedings of the Fourth Conference on Stably Stratified Flows, organized by the Institute of Mathematics and Its Applications and held at the University of Surrey in September, 1992 / | 1 |
| QC880.4.B65 S784 1988 | An introduction to boundary layer meteorology / | 1 |
| QC880.4.B65 V55 2015 | Atmospheric boundary layer : integrating air chemistry and land interactions / | 2 |
| QC880.4.C64 |
Geophysical convection dynamics / Cloud-resolving modeling of convective processes / |
2 |
| QC880.4 .C64 | Cloud-resolving modeling of convective processes | 1 |
| QC880.4.C64 A76 2007 | Atmospheric convection research and operational forecasting aspects / | 1 |
| QC880.4.C64 A84 2007 | Atmospheric convection : research and operational forecasting aspects / | 1 |
| QC880.4.C64 C55 | Climate Dynamics : Why Does Climate Vary? | 1 |
| QC880.4.C64 C55 2010 | Climate dynamics : why does climate vary? / | 2 |
| QC880.4.C64 E5 1994 | Atmospheric convection / | 1 |
| QC880.4.C64 G36 2008 | Cloud-resolving modeling of convective processes / | 1 |
| QC880.4.C64 M85 2017 | Multiscale convection-coupled systems in the tropics : a tribute to Dr. Michio Yanai / | 1 |
| QC880.4.C64 P59 1997 | The physics and parameterization of moist atmospheric convection / | 1 |
| QC880.4.C64 S484 2001 | Severe convective storms / | 1 |
| QC880.4.C64 S49 2001 | Severe convective storms | 1 |
| QC880.4.C65 S76 1989 | An introduction to the Coriolis force / | 2 |
