Articles | Volume 16, issue 1
https://doi.org/10.5194/acp-16-161-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-16-161-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The diurnal cycle of rainfall over New Guinea in convection-permitting WRF simulations
M. E. E. Hassim
CORRESPONDING AUTHOR
School of Earth Sciences and ARC Centre of Excellence for Climate System Science, The University of Melbourne, Melbourne, Victoria, 3010, Australia
now at: Centre for Climate Research Singapore, Meteorological Service Singapore, Singapore
T. P. Lane
School of Earth Sciences and ARC Centre of Excellence for Climate System Science, The University of Melbourne, Melbourne, Victoria, 3010, Australia
W. W. Grabowski
National Center for Atmospheric Research, Boulder, Colorado, USA
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74 citations as recorded by crossref.
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- Evaluation of multi-season convection-permitting atmosphere – mixed-layer ocean simulations of the Maritime Continent E. Howard et al. 10.5194/gmd-17-3815-2024
- Convection‐permitting modeling with regional climate models: Latest developments and next steps P. Lucas‐Picher et al. 10.1002/wcc.731
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Latest update: 21 Nov 2024
Short summary
Gravity waves from deep convection along with terrain and coastal effects control the development and movement of squall lines that affect the diurnal cycle of rainfall over New Guinea and its northern coast. Days with offshore propagating systems are governed by background conditions (more mid-tropospheric moisture, CAPE, and low-level convergence) as opposed to days without offshore propagation. Our results shed some light on the physics and dynamics of Maritime Continent organised convection
Gravity waves from deep convection along with terrain and coastal effects control the...
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