Assessing ecological health of mangrove ecosystems along South China Coast by the pressure–state–response (PSR) model

Ecotoxicology ◽  
2021 ◽  
Vol 30 (4) ◽  
pp. 622-631
Author(s):  
Yu-Tu Wang ◽  
You-Shao Wang ◽  
Mei-Lin Wu ◽  
Cui-Ci Sun ◽  
Ji-Dong Gu
Keyword(s):  
South China ◽  
Ecological Health ◽  
State Response ◽  
Mangrove Ecosystems ◽  
South China Coast ◽  
China Coast ◽  
Pressure State

Dynamic Geomorphic Systems of South China Coast

1994 ◽  
pp. 465-476
Author(s):  
Yuan Jia-Yi ◽  
Zhao Huan-Ting ◽  
Lu Tie-Song ◽  
Chao-jing Song ◽  
Zhang Qiao-Min
Keyword(s):  
South China ◽  
South China Coast ◽  
China Coast

Health risk assessment of heavy metal and its mitigation by glomalin-related soil protein in sediments along the South China coast

2020 ◽  
Vol 263 ◽  
pp. 114565
Author(s):  
Qiang Wang ◽  
Hualong Hong ◽  
Dan Yang ◽  
Junwei Li ◽  
Shan Chen ◽  
...  
Keyword(s):  
Risk Assessment ◽  
Heavy Metal ◽  
Health Risk ◽  
Health Risk Assessment ◽  
South China ◽  
The South ◽  
South China Coast ◽  
China Coast ◽  
Soil Protein

The South China coast in French and Dutch literature

2011 ◽  
Vol 6 (3) ◽  
pp. 407-422
Author(s):  
Ellen Xiangyu Cai
Keyword(s):  
South China ◽  
The South ◽  
South China Coast ◽  
Dutch Literature ◽  
China Coast

Distribution of convection associated with tropical cyclones making landfall along the South China coast

2007 ◽  
Vol 97 (1-4) ◽  
pp. 57-68 ◽  
Author(s):  
K. S. Liu ◽  
J. C. L. Chan ◽  
W. C. Cheng ◽  
S. L. Tai ◽  
P. W. Wong
Keyword(s):  
Tropical Cyclones ◽  
South China ◽  
The South ◽  
South China Coast ◽  
China Coast

scholarly journals A Simple Empirical Model for Estimating the Intensity Change of Tropical Cyclones after Landfall along the South China Coast

2008 ◽  
Vol 47 (1) ◽  
pp. 326-338 ◽  
Author(s):  
Martin L. M. Wong ◽  
Johnny C. L. Chan ◽  
Wen Zhou
Keyword(s):  
Tropical Cyclones ◽  
Exponential Decay ◽  
South China ◽  
Surface Wind ◽  
Decay Rates ◽  
Central Pressure ◽  
Intensity Change ◽  
The South ◽  
South China Coast ◽  
China Coast

Abstract The intensity change of past (1976–2005) tropical cyclones that made landfall along the south China coast (110.5°–117.5°E) is examined in this study using the best-track data from the Hong Kong Observatory. The change in the central pressure deficit (environmental pressure minus central pressure) and maximum surface wind after landfall are found to fit fairly well with an exponential decay model. Of the various potential predictors, the landfall intensity, landward speed, and excess of 850-hPa moist static energy have significant influence on the decay rates. Prediction equations for the exponential decay constants are developed based on these predictors.

Predominant factors of disaster caused by tropical cyclones in South China coast and implications for early warning systems

2020 ◽  
Vol 726 ◽  
pp. 138556 ◽  
Author(s):  
Linlin Wang ◽  
Yun Zhou ◽  
Xiaoyu Lei ◽  
Yanyan Zhou ◽  
Hongsheng Bi ◽  
...  
Keyword(s):  
Tropical Cyclones ◽  
South China ◽  
Early Warning ◽  
Early Warning Systems ◽  
Warning Systems ◽  
South China Coast ◽  
China Coast

The Crucial Role of Synoptic Pattern in Determining the Spatial Distribution and Diurnal Cycle of Heavy Rainfall over the South China Coast

2020 ◽  
pp. 1-47
Author(s):  
Chenli Wang ◽  
Kun Zhao ◽  
Anning Huang ◽  
Xingchao Chen ◽  
Xiaona Rao
Keyword(s):  
South China ◽  
Heavy Rainfall ◽  
Warm Season ◽  
Early Morning ◽  
The South ◽  
Synoptic Patterns ◽  
Low Level ◽  
South China Coast ◽  
China Coast

AbstractSouth China coast suffers frequent heavy rainfall every warm-season. Based on the objective classification method of principle components analysis, the key role of synoptic pattern in determining the heavy rainfall processes occurred over the South China coast in warm season during 2008-2018 is examined in this study. We found heavy rainfall occurs most frequently under three typical synoptic patterns (P1-P3 hereafter) characterized by strong low-level onshore winds. P1 and P3 are featured by a prevailing southwesterly monsoonal flow in the lower troposphere, with heavy rainfall frequently occurring over the inland windward region in the afternoon associated with the orographic lifting and solar heating. The onshore wind of P3 is stronger than P1 as the western Pacific subtropical high extends more westward to 122°E, which induces stronger low-level convergence along the coastline than P1 when the ageostrophic wind veers from offshore to onshore direction in the early morning. Hence, a secondary early morning rainfall peak can be found along the coastline. P2 is characterized by a low-level vortex located over the southwest of south China. Heavy rainfall under P2 usually initiate over the western part of the coastal region in the morning and then propagate towards inland in the afternoon. Overall, the synoptic patterns strongly determine the spatial distribution and diurnal cycle of heavy rainfall over the South China coast. It is closely related to the diurnally varying low-level onshore winds rather than the low-level jets, as well as the different interactions between the low-level onshore winds and the local orography, coastline and land-sea breeze circulations under different synoptic patterns.

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