Chotika Maungsong
Biographic Data
| ID | 242982 |
|---|---|
| NAME | Chotika Maungsong |
| GIVEN NAMES | Chotika |
| FAMILY NAME | Maungsong |
| SIGNATURE | MAUNGSONG C |
| AFFILIATIONS | Fujian Normal University |
| ORCID | 0000-0001-7956-5191 |
| VERIFIED | Yes |
| TOTAL WORKS | 5 |
| TOTAL CITATIONS | 2 |
| WORKS AS AUTHOR | 5 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2014 |
| LATEST PUBLICATION YEAR | 2022 |
| H-INDEX | 1 |
Tree-ring oxygen isotope chronology of teak log coffins in northwestern Thailand and its relationship with Pacific Decadal Oscillation and El Niño-Southern Oscillation
Inter-annual and intra-annual tree-ring oxygen isotope signals in response to monsoon rainfall in northwestern Thailand
We present a new teak ( Tectona grandis L.f.) tree-ring stable oxygen isotope (δ 18 O TR ) chronology from Mae Tuen (MT) site, Tak province, northwestern Thailand at inter-annual (167-year, A.D.1850–2016) and intra-annual (A.D.2006–2016) timescales. The inter-annual δ 18 O TR chronology showed a significant negative correlation ( r = −0.678, p < 0.01) with the May–October amount of regional rainfall obtained from CRU TS4.03. We established a line…
The potential of teak log coffins collected from Namjang Cave in Northwestern Thailand for studying the coffin culture and paleoclimate in Southeast Asia
Intra-seasonal variability of teak tree-ring cellulose δ 18 O from northwestern Thailand
Thailand has been regarded as a transition zone between the Indian and western North Pacific monsoons which produce most of the precipitation in this area and sustain large-scale agricultural activities. Their different moisture sources and associated transport trajectories could result in distinguishable seasonal variations in rainfall oxygen isotopes (δ 18 O). Knowledge about seasonal variability in Thailand monsoon could facilitate agricultura…
An annually laminated stalagmite record of the changes in Thailand monsoon rainfall over the past 387 years and its relationship to IOD and Enso
The potential of teak log coffins collected from Namjang Cave in Northwestern Thailand for studying the coffin culture and paleoclimate in Southeast Asia
Intra-seasonal variability of teak tree-ring cellulose δ 18 O from northwestern Thailand
Thailand has been regarded as a transition zone between the Indian and western North Pacific monsoons which produce most of the precipitation in this area and sustain large-scale agricultural activities. Their different moisture sources and associated transport trajectories could result in distinguishable seasonal variations in rainfall oxygen isotopes (δ 18 O). Knowledge about seasonal variability in Thailand monsoon could facilitate agricultura…
An annually laminated stalagmite record of the changes in Thailand monsoon rainfall over the past 387 years and its relationship to IOD and Enso
Intra-seasonal variability of teak tree-ring cellulose δ 18 O from northwestern Thailand
Thailand has been regarded as a transition zone between the Indian and western North Pacific monsoons which produce most of the precipitation in this area and sustain large-scale agricultural activities. Their different moisture sources and associated transport trajectories could result in distinguishable seasonal variations in rainfall oxygen isotopes (δ 18 O). Knowledge about seasonal variability in Thailand monsoon could facilitate agricultura…
The potential of teak log coffins collected from Namjang Cave in Northwestern Thailand for studying the coffin culture and paleoclimate in Southeast Asia
Tree-ring oxygen isotope chronology of teak log coffins in northwestern Thailand and its relationship with Pacific Decadal Oscillation and El Niño-Southern Oscillation
Inter-annual and intra-annual tree-ring oxygen isotope signals in response to monsoon rainfall in northwestern Thailand
We present a new teak ( Tectona grandis L.f.) tree-ring stable oxygen isotope (δ 18 O TR ) chronology from Mae Tuen (MT) site, Tak province, northwestern Thailand at inter-annual (167-year, A.D.1850–2016) and intra-annual (A.D.2006–2016) timescales. The inter-annual δ 18 O TR chronology showed a significant negative correlation ( r = −0.678, p < 0.01) with the May–October amount of regional rainfall obtained from CRU TS4.03. We established a line…
Geography (5 works) · Geology (5 works) · Climatology (4 works) · Geology and Paleoclimatology Research (4 works) · Monsoon (4 works) · Dendrochronology (3 works) · Oceanography (3 works) · Precipitation (3 works) · Stalagmite (3 works) · Tree-ring climate responses (3 works)