The Maritime Continent and Its Role in the Global Climate: A GCM Study
Top Cited Papers
- 1 March 2003
- journal article
- Published by American Meteorological Society in Journal of Climate
- Vol. 16 (5) , 834-848
- https://doi.org/10.1175/1520-0442(2003)016<0834:tmcair>2.0.co;2
Abstract
The Maritime Continent, with its complex system of islands and shallow seas, presents a major challenge to models, which tend to systematically underestimate the precipitation in this region. Experiments with a climate version of the Met Office model (HadAM3) show that even with a threefold increase in horizontal resolution there is no improvement in the dry bias. It is argued that the diurnal cycle over the islands and the complex circulation patterns generated by land–sea contrasts are crucial for the energy and hydrological cycles of the Maritime Continent and for determining the mean climate. It is shown that the model has substantial errors in its simulation of the diurnal cycle over the islands, which can rectify onto the seasonal mean climate. It is further argued that deficient rainfall over the Maritime Continent could be a driver for other systematic errors, such as the excess precipitation over the western Indian Ocean. To demonstrate the sensitivity of global systematic model errors t... Abstract The Maritime Continent, with its complex system of islands and shallow seas, presents a major challenge to models, which tend to systematically underestimate the precipitation in this region. Experiments with a climate version of the Met Office model (HadAM3) show that even with a threefold increase in horizontal resolution there is no improvement in the dry bias. It is argued that the diurnal cycle over the islands and the complex circulation patterns generated by land–sea contrasts are crucial for the energy and hydrological cycles of the Maritime Continent and for determining the mean climate. It is shown that the model has substantial errors in its simulation of the diurnal cycle over the islands, which can rectify onto the seasonal mean climate. It is further argued that deficient rainfall over the Maritime Continent could be a driver for other systematic errors, such as the excess precipitation over the western Indian Ocean. To demonstrate the sensitivity of global systematic model errors t...Keywords
This publication has 31 references indexed in Scilit:
- Simulation of the Madden–Julian Oscillation in a Coupled General Circulation Model. Part I: Comparison with Observations and an Atmosphere-Only GCMJournal of Climate, 2003
- Coupling Cloud Processes with the Large-Scale Dynamics Using the Cloud-Resolving Convection Parameterization (CRCP)Journal of the Atmospheric Sciences, 2001
- Predictable winter climate in the North Atlantic sector during the 1997–1999 ENSO cycleGeophysical Research Letters, 2000
- The impact of new land surface physics on the GCM simulation of climate and climate sensitivityClimate Dynamics, 1999
- Studies with a flexible new radiation code. I: Choosing a configuration for a large‐scale modelQuarterly Journal of the Royal Meteorological Society, 1996
- AMIP: The Atmospheric Model Intercomparison ProjectBulletin of the American Meteorological Society, 1992
- A Mass Flux Convection Scheme with Representation of Cloud Ensemble Characteristics and Stability-Dependent ClosureMonthly Weather Review, 1990
- Short-Term Planetary-Scale Interactions over the Tropics and Midlatitudes during Northern Winter. Part I: Contrasts between Active and Inactive PeriodsMonthly Weather Review, 1982
- Winter Monsoon Convection in the Vicinity of North Borneo. Part I: Structure and Time Variation of the Clouds and PrecipitationMonthly Weather Review, 1981
- Diurnal Variations of Convection over the “Maritime Continent”Monthly Weather Review, 1980