2019
DOI: 10.1007/s13131-019-1369-7
|View full text |Cite
|
Sign up to set email alerts
|

Dynamic of ENSO towards upwelling and thermal front zone in the east coast of Peninsular Malaysia

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2019
2019
2022
2022

Publication Types

Select...
4

Relationship

0
4

Authors

Journals

citations
Cited by 4 publications
(1 citation statement)
references
References 20 publications
0
1
0
Order By: Relevance
“…While drought indices are highly depending on precipitation amount, over Peninsular Malaysia, precipitation variability is primarily driven by monsoons (Fung et al, 2020a;Suhaila et al, 2010), which show large variability from 1 year to another in response to changes in ocean-atmospheric modes of climate variability (Albani et al, 2018;Supari et al, 2018;Tangang et al, 2012). The hydroclimate variability over Malaysia has been found to be affected by sea surface temperature (SST) variability, especially over the Pacific Ocean (e.g., Daud et al, 2019;Salimun et al, 2014;Suhaila et al, 2010;Tangang & Juneng, 2004) and the Indian Ocean (e.g., Tan et al, 2017;Tangang et al, 2008Tangang et al, , 2012. Furthermore, in both the Pacific and Indian oceans, SST variability has been linked to processes modulating the moisture distribution in the troposphere (Chakraborty et al, 2006;Lee et al, 2015;Pillai & Mohankumar, 2010).…”
Section: Introductionmentioning
confidence: 99%
“…While drought indices are highly depending on precipitation amount, over Peninsular Malaysia, precipitation variability is primarily driven by monsoons (Fung et al, 2020a;Suhaila et al, 2010), which show large variability from 1 year to another in response to changes in ocean-atmospheric modes of climate variability (Albani et al, 2018;Supari et al, 2018;Tangang et al, 2012). The hydroclimate variability over Malaysia has been found to be affected by sea surface temperature (SST) variability, especially over the Pacific Ocean (e.g., Daud et al, 2019;Salimun et al, 2014;Suhaila et al, 2010;Tangang & Juneng, 2004) and the Indian Ocean (e.g., Tan et al, 2017;Tangang et al, 2008Tangang et al, , 2012. Furthermore, in both the Pacific and Indian oceans, SST variability has been linked to processes modulating the moisture distribution in the troposphere (Chakraborty et al, 2006;Lee et al, 2015;Pillai & Mohankumar, 2010).…”
Section: Introductionmentioning
confidence: 99%