Citation

BibTex format

@article{Tsui:2026:2515-7620/aeaad1,
author = {Tsui, EYL and Toumi, R and Satoh, M},
doi = {2515-7620/aeaad1},
journal = {Environmental Research Communications},
pages = {101012--101012},
title = {On the precipitation of seafalling tropical cyclones crossing the Philippines},
url = {http://dx.doi.org/10.1088/2515-7620/aeaad1},
volume = {8},
year = {2026}
}

RIS format (EndNote, RefMan)

TY  - JOUR
AB - <jats:title>Abstract</jats:title> <jats:p> The precipitation of tropical cyclones crossing the Philippines between 2001 and 2022 is analysed over the <jats:inline-formula> <jats:tex-math> </jats:tex-math> <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <mml:mrow> <mml:mn>9</mml:mn> </mml:mrow> </mml:math> </jats:inline-formula> h periods before the cyclone makes landfall and after it then re-enters the ocean (‘seafall’). Precipitation is favoured over the land side for landfalling storms. However, the precipitation from a seafalling storm is more spread out and asymmetric on the ocean side. When adjusted for intensity, seafall storms have a larger total precipitation rate than landfall storms by <jats:inline-formula> <jats:tex-math> </jats:tex-math> <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <mml:mrow> <mml:mn>25</mml:mn> <mml:mi mathvariant="normal">%</mml:mi> </mml:mrow> </mml:math> </jats:inline-formula> . The precipitation pattern in the landfalling storms appears to be the result of both orography and land–sea frictional and thermal contrasts. Seafalling storm precipitation anomalies are likely caused by a local boost in surface heat and moisture supply from the oc
AU - Tsui,EYL
AU - Toumi,R
AU - Satoh,M
DO - 2515-7620/aeaad1
EP - 101012
PY - 2026///
SP - 101012
TI - On the precipitation of seafalling tropical cyclones crossing the Philippines
T2 - Environmental Research Communications
UR - http://dx.doi.org/10.1088/2515-7620/aeaad1
UR - https://doi.org/10.1088/2515-7620/aeaad1
VL - 8
ER -

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