Model comparison for estimating cloud liquid water content and attenuation in tropical region

Yuan, Feng; Manandhar, Shilpa; Lee, Yee Hui; Meng, Yu Song

doi:10.1109/tencon.2016.7848226

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Special Case For Convective Rain1

Dierentiation Between Stratiform and Convective Rain1

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“…This represents a heavy convective rain event and the rain cell height extends up to above 6 km. This height is around 1 km higher than the average 0°C isotherm heights which is reported in [91] to be within [4.2 km, 5.5 km] (processed from one-year radiosonde temperature vertical proles in Singapore [91]). In [27] [92] [93], it was reported that the 0°C isotherm height is close to the top boundary of the melting layer and the rain height.…”

Section: Special Case For Convective Rainmentioning

confidence: 51%

“…After classifying all the slant rays, a clear separation of the stratiform rain cell and the convective rain cell from for a convective rain cell in the tropical region. In [91], the 0°C isotherm heights for tropical region are reported to be typically within the range of [4.2 km, 5.5 km]. It is reported in [27] [92] [93] that the 0°C isotherm height is generally taken as the top boundary of melting layers.…”

Section: Dierentiation Between Stratiform and Convective Rainmentioning

confidence: 99%

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