Abstract
Deepmoist 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 rainfall, and predicting such convection is therefore critical for both disaster prevention and climate projection. Although the key parameters for convection have been pointed out, understanding the preprocesses of convection is a challenging issue. Here we identified the precursors of convection by analyzing a global simulated data set with very high resolution in time and space. We found that the mass convergence near the Earth’s surface changed significantly several minutes before the initiation of early convection (the formation of cumulus clouds), which occurred with the increase in the convective available potential energy (CAPE). Decomposition of the statistical data revealed that a higher-CAPE environment resulted in stronger convection than in the stronger-convergence case. Furthermore, for the stronger-convergence case, the precursor was detected earlier than the total average (10-15 min before the initiation), whereas the amplitude of maximum velocity was not so strong as the higher-CAPE case. This suggests that the strength of convection is connected with CAPE, and the predictability is sensitive to the convergence.
| Original language | English |
|---|---|
| Pages (from-to) | 12,080-12,088 |
| Journal | Journal of Geophysical Research |
| Volume | 121 |
| Issue number | 20 |
| DOIs | |
| Publication status | Published - 2016 Oct 27 |
| Externally published | Yes |
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ASJC Scopus subject areas
- Geophysics
- Forestry
- Oceanography
- Aquatic Science
- Ecology
- Water Science and Technology
- Soil Science
- Geochemistry and Petrology
- Earth-Surface Processes
- Atmospheric Science
- Earth and Planetary Sciences (miscellaneous)
- Space and Planetary Science
- Palaeontology
Cite this
Precursors of deep moist convection in a subkilometer global simulation. / Miyamoto, Yoshiaki; Yamaura, Tsuyoshi; Yoshida, Ryuji; Yashiro, Hisashi; Tomita, Hirofumi; Kajikawa, Yoshiyuki.
In: Journal of Geophysical Research, Vol. 121, No. 20, 27.10.2016, p. 12,080-12,088.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Precursors of deep moist convection in a subkilometer global simulation
AU - Miyamoto, Yoshiaki
AU - Yamaura, Tsuyoshi
AU - Yoshida, Ryuji
AU - Yashiro, Hisashi
AU - Tomita, Hirofumi
AU - Kajikawa, Yoshiyuki
PY - 2016/10/27
Y1 - 2016/10/27
N2 - Deepmoist 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 rainfall, and predicting such convection is therefore critical for both disaster prevention and climate projection. Although the key parameters for convection have been pointed out, understanding the preprocesses of convection is a challenging issue. Here we identified the precursors of convection by analyzing a global simulated data set with very high resolution in time and space. We found that the mass convergence near the Earth’s surface changed significantly several minutes before the initiation of early convection (the formation of cumulus clouds), which occurred with the increase in the convective available potential energy (CAPE). Decomposition of the statistical data revealed that a higher-CAPE environment resulted in stronger convection than in the stronger-convergence case. Furthermore, for the stronger-convergence case, the precursor was detected earlier than the total average (10-15 min before the initiation), whereas the amplitude of maximum velocity was not so strong as the higher-CAPE case. This suggests that the strength of convection is connected with CAPE, and the predictability is sensitive to the convergence.
AB - Deepmoist 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 rainfall, and predicting such convection is therefore critical for both disaster prevention and climate projection. Although the key parameters for convection have been pointed out, understanding the preprocesses of convection is a challenging issue. Here we identified the precursors of convection by analyzing a global simulated data set with very high resolution in time and space. We found that the mass convergence near the Earth’s surface changed significantly several minutes before the initiation of early convection (the formation of cumulus clouds), which occurred with the increase in the convective available potential energy (CAPE). Decomposition of the statistical data revealed that a higher-CAPE environment resulted in stronger convection than in the stronger-convergence case. Furthermore, for the stronger-convergence case, the precursor was detected earlier than the total average (10-15 min before the initiation), whereas the amplitude of maximum velocity was not so strong as the higher-CAPE case. This suggests that the strength of convection is connected with CAPE, and the predictability is sensitive to the convergence.
UR - http://www.scopus.com/inward/record.url?scp=84995595410&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84995595410&partnerID=8YFLogxK
U2 - 10.1002/2016JD024965
DO - 10.1002/2016JD024965
M3 - Article
AN - SCOPUS:84995595410
VL - 121
SP - 12,080-12,088
JO - Journal of Geophysical Research
JF - Journal of Geophysical Research
SN - 0148-0227
IS - 20
ER -