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Chawalit ". Charoenpong on Muck Rack

Chawalit ". Charoenpong

As seen in: Frontiers, Frontiers in Marine Science, Open Quaternary Journal
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Articles

Frontiers | Correction: Physico-biochemical controls on dissolved oxygen dynamics in the Eastern Upper Gulf of Thailand: field observations and numerical modeling

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By Phatcharaporn Kaewkhong, Tanuspong Pokavanich, Kanokwan Khaodon, Chawalit ". Charoenpong
| Frontiers in Marine Science
CORRECTION article Volume 13 - 2026 | https://doi.org/10.3389/fmars.2026.1786090 There was a mistake in Figure 1 as published. The legend explaining the symbols in the figure was incomplete. The corrected Figure 1 appears below. Figure 1. Map of the Upper Gulf of Thailand (UGoT) showing (A) the study area, major riverine inputs (Bang Pakong, Chao Phraya, Tha Chin, and Mae Klong), the location of the GOT001 station, and the 6-monthly sampling stations.
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Physico-biochemical controls on dissolved oxygen dynamics in the Eastern Upper Gulf of Thailand: field observations and numerical modeling

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By Tanuspong Pokavanich, Kanokwan Khaodon, Chawalit ". Charoenpong, Phatcharaporn Kaewkhong
| Frontiers in Marine Science
1 Introduction Hypoxia, typically defined as dissolved oxygen (DO) concentrations below 2 mg L−¹ (Diaz, 2001), is a pervasive problem in aquatic systems and causes severe ecological impacts, including mass fish mortality, habitat degradation, and altered marine community structure (Diaz and Rosenberg, 2008; Vaquer-Sunyer and Duarte, 2008; Dai et al., 2023).
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Hydroclimate Variability in the Mainland Southeast Asia During the Last Glacial Maximum

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By Chawalit ". Charoenpong, Akkaneewut Jirapinyakul, Dissaya Sukaudom, Penjai Sompongchaikul
| Open Quaternary Journal Verified
Research paper Akkaneewut Jirapinyakul Dissaya Sukaudom Chawalit Charoenpong Penjai Sompongchaikul Paramita Punwong Kweku Afrifa Yamoah The Last Glacial Maximum (LGM) is a key reference point for understanding past climate, but its complexity can lead to ambiguities in scope and interpretation. In this study, we applied a suite of geochemical techniques -XRF, grain size, and pollen analysis- to a well-dated sedimentary sequence from the lower central plain of Thailand.
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