| Summary: | The knowledge of soil apparent thermal diffusivity (k) is important for investigating soil surface heat transfer and temperature. Long-term k determined using the near-surface soil temperature is limited on the Tibetan Plateau (TP). The main objective of this study is to determine k with a conduction–convection method using the near-surface soil temperature measured at three sites during 2014–2016 on the TP. The hourly, daily, and monthly k values of the 0.0 m to 0.20 m layer were obtained. The hourly and daily k values ranged from 0.3 × 10<sup>−6</sup> m<sup>2</sup> s<sup>−1</sup> to 1.9 × 10<sup>−6</sup> m<sup>2</sup> s<sup>−1</sup> at the wet site, and from 1.0 × 10<sup>−7</sup> m<sup>2</sup> s<sup>−1</sup> to 4.0 × 10<sup>−7</sup> m<sup>2</sup> s<sup>−1</sup> at the two dry sites. For the monthly timescale, k ranged from 0.4 (±0.0) × 10<sup>−6</sup> m<sup>2</sup> s<sup>−1</sup> to 1.1 (±0.2) × 10<sup>−6</sup> m<sup>2</sup> s<sup>−1</sup> at the wet site, and varied between 1.7 (±0.0) × 10<sup>−7</sup> m<sup>2</sup> s<sup>−1</sup> and 3.3 (±0.2) × 10<sup>−7</sup> m<sup>2</sup> s<sup>−1</sup> at the two dry sites. The k was not constant over a day, and it varied seasonally to different degrees at different sites and years. The variation of k with soil moisture (θ) appeared to be roughly similar for unfrozen soil at these sites and years, namely, k increased sharply before reaching the peak as θ increased, and then it tended to be stable or varied slightly with further increases in θ. This variation trend was consistent with previous studies. However, the relationship between k and θ changed when soil temperature was below 0 °C, because ice had higher k than water. The correlation coefficients (r) between k and θ ranged from 0.37 to 0.80, and 0.80 to 0.92 on hourly and monthly timescales, respectively. The monthly and annual k values were significantly correlated (r: 0.73~0.93) to the Normalized Difference Vegetation Index (NDVI). The results broaden our understanding of the relationship between in situ k and θ. The presented values of k at various timescales can be used as soil parameters when modeling land–atmosphere interactions at these TP regions.
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