JAPRS & SIS, Vol.34, Part 7, “Resource and Environmental Monitoring”, Hyderabad, India, 2002
(Amreli)
63 aat T € — n
1 (slope =-40.384) |
0.701 02-03 04-05
NDVI
50 (slope =-28.3010 |
Figure 1: A scatterogram between LST and NDVI
on 15 january 1999
that high NDVI was associated with low LST over more
densely vegetated areas(Kheda and Banaskantha), generally
during the peak growing season (i.e January ) as compared to
sparsely vegetated area (Amreli and Rajkot). Greater scatter
and steeper slopes was also observed for Amreli and Rajokt
than Kheda and Banaskantha districts. These differences in
slope were related to vegetation physiological control as the
partitioning of net radiation into latent heat and sensible heat
fluxes with steeper slopes for the sites with reduced soil
moisture and vegetation amount. The small differences in LST
at large NDVI (i.e >0.3) between densely vegetated areas
(Kheda and Banaskantha) could be attributed to variation in
LST being causefl by factors such as spatially variable
meteorological conditions, physiological and architectural
differences in the plants and the variations in the terrain
resulting in site to site differences in insolation.
The AVHRR-LAC derived LST versus NDVI relationship for
four dates in 1998-99 (figure 2) that characterize most of the
variability through the growing seasons of mustard, the
dominant crop of Banaskantha district. Differences between
slope of regression may be ascribed to soil moisture and
vegetational evaporative fraction, with the steeper slope during
mid growth stages (i.e January 15 (slope=-31.019)) and
(February 18 (Slope=-28.301)) and shallowest slope during
early (December 15(Slope=-37.061)) and late (March 17
(Slope=-43.517)) stages. The regression lines for all four dates
converged as the NDVI approached a value of 0.4. Nemani and
(Rajkot)
(sope = -36.941)
0 01---02-<0:3-—-04-—05
NDVI
(slope z -43.517)
LST(C)
0 0.1 0.2 03 04 05
Figure 2 : A scatterogarm between LST and NDVI for
Banaskantha Distric (a)15 Dec, 1998, (b) 15 Jan., 1999,
( c) 18 Feb., 199 (d) 17 Mar., 1999
Running (1989) observed a similar phenomenon and found that
the Ts-NDVI regressions calculated for two different dates over
a conifer stand had different slope but converged as the NDVI
approached the maximum observed value. The spread of
scatterogram also observed to increase with progress of crop
growth and fractional vegetation cover. Greater scatter was
noticed during the early and late growing stages of rabi crop
growing season of mustard in Banaskantha.
4.3 Validations of surface meteorological parameters
Validation of surface land surface land temperatures derived
from the satellite data was done using in-situ measurements of
soil temperatures (5,10 and 20 cm depth) at 14.30h IST from
three agro meteorological stations, over dates of satellite
overpass. These soil temperatures were extrapolated to obtain
the soil surface temperatures using statistical regression model.
The comparison of observed satellite temperature and satellite
retrieved surface temperature is shown in table 2. A good
agreement was observed between satellite retrieved surface
temperature and with ground estimates of mid-day surface soil
temperatures. Satellite retrieved surface temperatures matching
with observed soil surface temperatures within 0.0 to 1.7°C, 0.2
to 2.1°C and 0.2 to 2.3°C for S.K.Nagar, Narsari and Godhara,
respectively. This shows that average bias in retrieved surface
temperature compared with observed surface soil temperature is
approximately 2°C or less over three meteorological stations for
all dates. Figure 3 shows
Table 2 :Comparison of satellite derived surface temperature with observed surface soil temperatures (14.30 IST)
December 31, 1998 January 15, 1999 February 18, 1999 March 17, 1999
Met. Station
Retrieved Observed Retrieved Observed Retrieved Observed Retrieved Observed
(°C) (°C) (°C) (C) (CC) °C) CC) (°C)
Godhara 30.23 30.0 32.5 30.2 37.6 36.4 41.7 43.0
Navsari 32.2 NA 30.1 28.0 36.6 35.0 38.8 39.0
SK Nagar 30.7 30.7 31.8 30.1 36.2 35.2 41.9 41.6
NA: Observed data not available
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