The physical processes causing nocturnal rainfall over northwest Australia and their representation in high‐ and low‐resolution models with parametrized convection-Reference-Cited by-同舟云学术

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The physical processes causing nocturnal rainfall over northwest Australia and their representation in high‐ and low‐resolution models with parametrized convection

Published:2018-01 Issue:711 Volume:144 Page:511-528
ISSN:0035-9009
Container-title:Quarterly Journal of the Royal Meteorological Society
language:en
Short-container-title:Q.J.R. Meteorol. Soc.

Author:

Ackerley D.¹,Birch C. E.²³,Garcia‐Carreras L.²,Lavender S. L.⁴,Weller E.¹

Affiliation:

1. ARC Centre of Excellence for Climate System Science, Monash University, Clayton, Victoria, Australia

2. School of Earth and Environment, University of Leeds, UK

3. MetOffice@Leeds, University of Leeds, UK

4. CSIRO Climate Science Centre, Aspendale, Victoria, Australia

Funder

Australian Research Council Centre of Excellence for Climate System Science

Australian Government

Publisher

Wiley

Subject

Atmospheric Science

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/qj.3223

Reference54 articles.

1. The roles of diurnal forcing and large-scale moisture transport for initiating rain over northwest Australia in a GCM

2. Summertime precipitation over northern Australia in AMIP simulations from CMIP5

3. Representing the Australian Heat Low in a GCM Using Different Surface and Cloud Schemes

4. The Diurnal and Seasonal Variation of the Northern Australian Dryline

5. The structure and evolution of the northern Australian dryline

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