(TVDI) COMPUTATION FOR DROUGHTS PHASE MAPPING USING REMOTE SENSING DATA

TEMPERATURE VEGETATION DRYNESS INDEX
(TVDI) COMPUTATION FOR DROUGHTS PHASE
MAPPING USING REMOTE SENSING DATA
(CASE STUDY: TAMAN NASIONAL BROMO TENGGER
SEMERU)
Name of Student
NRP
Department
Supervisor
:
:
:
:
Ahmad Azhar Ibrahimi
3509 100 034
Teknik Geomatika FTSP-ITS
Hepi Hapsari Handayani ST, M.Sc
Abstract
Droughts occur when a land area experiencing water
shortages. every dry season in Indonesia drought is almost
happen in forest with different intensity and areas each year, so
drought monitoring is important. In this research TVDI
(Temperature Vegetation Dryness Indeks) is used for monitoring
the droughts at forest area.Droughts Index is adjuted by land
surface temperature and vegetation index for reference.
In this research, NDVI (Normalized Difference Vegetation
Index) and LST (Land Surface Temperature) from ASTER DATA
are useful for developing The TVDI models.
The formulas that obtained from the research are TVDI= (LST
– (50.86*NDVI – 20.253))/((-114.248*NDVI) + 88.162). The
index range from The research are TVDI 0 – 0.2 (wet), 0.2 – 0.4
(dampy), 0.4 – 0.6 (normal), 0.6 – 0.8 (dryish), 0.8 – 1 (dry) The
extents of them are 3282.28 ha, 4263.19 ha, 8039.59 ha, 7156.46
ha, 2553.30 ha.
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