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Spatial Heterogeneity and Climate Correlates of Vegetation Greenness across Indonesian Provinces: Evidence from Multi-Source Remote Sensing and Panel Data (2018–2024)

Authors

  • Aman Suyadi Email ORCID Department ofAgrotechnology, Faculty ofAgriculture and Fisheries, Universitas Muhammadiyah Purwokerto, Purwokerto 53182, Indonesia
  • Marga Surya Mudhari ORCID Research Center for Photonics, National Research and Innovation Agency (BRIN), Jakarta 10340, Indonesia

DOI:

https://doi.org/10.30564/re.v8i5.117286

Received:6 August 2026 |Revised:15 September 2026 |Accepted:21 September 2026 |Published Online:16 October 2026

Abstract

Strong spatial associations between land surface temperature (LST) and vegetation greenness are often interpreted as evidence of vegetation responses to temperature. We examined whether that interpretation is supported by annual observations from 34 Indonesian provinces during 2018–2024 (238 province-year records). The Moderate Resolution Imaging Spectroradiometer (MODIS) normalized difference vegetation index (NDVI) and daytime land surface temperature (LST) were combined with Climate Hazards Group InfraRed Precipitation with Station data (CHIRPS) rainfall, TerraClimate Palmer Drought Severity Index (PDSI), and Soil Moisture Active Passive (SMAP) surface soil moisture. Pooled and fixed-effects (FE) regressions compared the national association with changes within provinces, while Moran’s I assessed remaining spatial structure. NDVI and LST were strongly inversely correlated (r = −0.845). After adjustment for rainfall, the LST coefficient was −0.03296 in pooled OLS and −0.00420 under province FE (p = 0.081), an 87.3% reduction in magnitude. Adding year effects gave a coefficient of −0.01035. Evidence for this within-province association was suggestive: province-clustered p = 0.021, but restricted wild-cluster bootstrap p = 0.076. Driscoll–Kraay inference gave p < 0.001, although its reliability is limited by the seven-year panel. One-year-lag coefficients were not distinguishable from zero. Two-way FE residuals remained spatially autocorrelated (Moran’s I = 0.227, p < 0.001). The main contribution is an empirical limit on using Indonesia’s provincial thermal–greenness gradient to infer interannual vegetation responses. Province means combine land-cover composition and canopy condition, and FE does not separate their changing contributions or resolve reciprocal LST–NDVI feedbacks. NDVI saturation and the absence of EVI or land-cover-stratified checks further restrict the ecological interpretation.

Keywords:

Vegetation Greenness, Remote Sensing, Normalized Difference Vegetation Index (NDVI), Land Surface Temperature, Panel Data, Spatial Autocorrelation, Indonesia

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