• Corpus ID: 45613060

N 0 . 2016-001 A simple method for detecting the lifecycle of deep moist convection from discretized data

@inproceedings{Miyamoto2016N0,
  title={N 0 . 2016-001 A simple method for detecting the lifecycle of deep moist convection from discretized data},
  author={Yoshiaki Miyamoto and Tsuyoshi Yamaura and Ryuji Yoshida and Hisashi Yashiro and Hirofumi Tomita and Yoshiyuki Kajikawa},
  year={2016}
}
Deep moist convection plays a crucial role in transporting energy and momentum in the Earth’s atmosphere. Examining the convection is fundamentally important for better understanding of various atmospheric phenomena, e.g., typhoons, as well as the convection itself. We developed a simple methodology for detecting the lifecycle of convection from discrete spatiotemporal data such as output of model simulations or reanalyses, which are often used in the Atmospheric Science research. The method… 

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References

SHOWING 1-7 OF 7 REFERENCES
Precursors of deep moist convection in a subkilometer global simulation
Deep moist convection in the atmosphere plays an important role in cloudy weather disturbances, such as hurricanes, and even in the global climate. The convection often causes disastrous heavy
Deep moist atmospheric convection in a subkilometer global simulation
Deep moist atmospheric convection is a key element of the weather and climate system for transporting mass, momentum, and thermal energy. It has been challenging to simulate convection realistically
Does convection vary in different cloud disturbances?
Deep moist convection is an element of cloud disturbances such as Madden‐Julian oscillation (MJO), tropical cyclones (TCs), mid‐latitudinal low depressions (MDL), and fronts (FRT). However,
Statistical properties of cloud lifecycles in cloud-resolving models
  • R. Plant
  • Environmental Science, Physics
  • 2008
TLDR
A new technique is described for the analysis of cloud-resolving model simulations, which allows one to investigate the statistics of the lifecycles of cumulus clouds, and an approach for handling cloud splits and mergers is described.
Direct entrainment and detrainment rate distributions of individual shallow cumulus clouds in an LES
Abstract. Probability distribution functions of shallow cumulus cloud core entrainment and detrainment rates are calculated using 4362 individual cumulus clouds isolated from LES (large eddy
Thermal Equilibrium of the Atmosphere with a Given Distribution of Relative Humidity
Abstract Radiative convective equilibrium of the atmosphere with a given distribution of relative humidity is computed as the asymptotic state of an initial value problem. The results show that it
Saturated-adiabatic ascent of air through dry-adiabatically descend
  • 1938