2009
DOI: 10.2151/sola.2009-011
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Spatial and Temporal Variations in Rainfall and the ENSO-rainfall Relationship over Sarawak, Malaysian Borneo

Abstract: To determine the spatial and temporal variations in the El Ni no Southern Oscillation (ENSO)-rainfall relationship and seasonal variation in rainfall over northern Borneo, simultaneous and lag correlations between the December February (DJF) average Ni no-3.4 (5°S 5°N, 170° 120°W) sea surface temperature (SST) and rainfall were examined using rainfall data from 18 stations throughout Sarawak during 1963 2003. The lag correlations for June August (JJA) rainfall and SST were significantly negative over southwest… Show more

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Cited by 17 publications
(6 citation statements)
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“…Complex Coupled Global Circulation Models suggest that ENSO frequency and magnitude under global warming are still unclear [37] . In addition, the ENSO–rainfall relationship may vary geographically, even within a region [38] , [39] . Further study is required to examine the combined effect of global climate change and ENSO on GF.…”
Section: Discussionmentioning
confidence: 99%
“…Complex Coupled Global Circulation Models suggest that ENSO frequency and magnitude under global warming are still unclear [37] . In addition, the ENSO–rainfall relationship may vary geographically, even within a region [38] , [39] . Further study is required to examine the combined effect of global climate change and ENSO on GF.…”
Section: Discussionmentioning
confidence: 99%
“…Monsoon and ENSO are two of the most influential forces modulating surface climate in the SE Asia (Dambul 2010). Previous studies in Indonesia and Malaysia, have established a significant relationship between rainfall variability and ENSO events (Aldrian & Susanto 2003;Chang et al 2004;Gomyo & Koichiro 2009;Tangang & Juneng 2004). To be more specific, positive correlation has been observed between SE Asia rainfall anomalies (SEAR) and ENSO evolution, where precipitation patterns are found to be highly affected by the irregular ENSO-related sea surface temperature (SST) anomalies (Juneng & Tangang 2005).…”
Section: Precipitation Anomalies-enso Eventmentioning
confidence: 97%
“…Additionally, several climate phenomena influence the local climate (i.e. temperature, rainfall, and river runoff), although to a lesser degree (Gomyo and Kuraji, 2009;Yan et al, 2015;Sa'adi et al, 2017b;Pan et al, 2018). These include the El Niño-Southern Oscillation (ENSO) creating dry (wet) conditions during El Niño (La Niña) (Murphy, 2006;Tangang et al, 2012), the Indian Ocean dipole creating cooler (warmer) conditions during positive (negative) phases and the Pacific Decadal Oscillation leading to colder (warmer) sea surface temperatures during the negative (positive) phase (Screen and Francis, 2016).…”
Section: Regional Setting and Climatementioning
confidence: 99%