The diurnal cycle of precipitation over the Maritime Continent in a high‐resolution atmospheric model

By Barnaby S Love, A. Matthews, G. Lister. 2011

209 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/effebc25aae97aaa4336d0361d50913f0e961ee8

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Bjorn Stevens
2. Chidong Zhang
3. C. DeMott
4. N. Klingaman
5. Á. Adames
6. E. Maloney
7. Daehyun Kim
8. Hai Lin

In Global and Planetary Change

1. Bjorn Stevens
2. Chidong Zhang
3. C. DeMott
4. N. Klingaman
5. Á. Adames
6. E. Maloney
7. Daehyun Kim
8. Hai Lin

Citations in the corpus

• The DOE E3SM Coupled Model Version 1: Description and Results at High Resolution (2019, background): “Sea breeze effects, which are important near the coasts in warm areas, also begin to be resolved as horizontal resolution improves (Boyle & Klein, 2010; Love et al., 2011).”
• Convection‐permitting modeling with regional climate models: Latest developments and next steps (2021, background): “The vast majority of studies using CPRCMs over islands have focused on rainfall (Love et al., 2011; Chan et al., 2013; Chan, Kahana, et al., 2018; Morel et al., 2014; Kendon et al., 2014; Fosser, Kendon, Stephenson, & Tucker, 2020; Dutheil et al., 2021) because it is directly affected by the way con”
• Large‐eddy simulations over Germany using ICON: a comprehensive evaluation (2017, background): “Thanks to increasing computational resources, increasingly larger domain cloud-resolving simulations are now possible (e.g. Hohenegger et al., 2008; Khairoutdinov et al., 2009; Love et al., 2011; Schlemmer and Hohenegger, 2014; Schalkwijk et al., 2015).”
• Fifty Years of Research on the Madden‐Julian Oscillation: Recent Progress, Challenges, and Perspectives (2020, background): “Due to land‐ocean contrasts and to complex topography over the mountainous MC islands, most of the total annual rainfall over the MC occurs via a vigorous diurnal cycle that is strongly coupled with land‐sea breezes (e.g., Kikuchi &Wang, 2008; Love et al., 2011; S. Mori et al., 2004; Nesbitt & Zipse”
• Propagation of the Madden–Julian Oscillation through the Maritime Continent and scale interaction with the diurnal cycle of precipitation (2014, background): “It should be noted that this effect is due not to the advection of storm clouds offshore, but to the triggering of gravity waves over the land which create new convection as they propagate away from their point of initiation (Love et al., 2011).”