Data from ocean color monitoring sensors at different spectral channels are available for remote sensing of radiation as seen in the given spectral windows, which is used for deriving information on various atmospheric parameters. However, recent studies have demonstrated the potential of hyperspectral (HS) data over multispectral ocean color (MSOC) data in accurately estimating phytoplankton concentration and in monitoring the coastal dynamics. We propose system spectral shape factor (SSSF)-based approach to recover the embedded HS top-of-atmosphere (TOA) radiance (TOARAD) from the MSOC data. SSSF is defined as convolution of normalized input spectrum and sensor spectral response function (SRF). The advantage of SSSF is that it decouples magnitude and spectral shape part of sensor output and enables recovery of TOARAD. To test this method, the airborne visible/infrared imaging spectrometer-next generation data are used to simulate inputs to MSOC. SRF of ocean color monitor simulated MSOC. SSSF of TOARAD is estimated using SSSF of model-based path radiance spectrum of the pixel, which is similar in spectral shape. Methodology, developed using data from five stations, is validated with data from other five stations. The procedure is successfully repeated using SRFs of sea-viewing wide-field-of-view sensor. The recovered HS data are found to be consistent with the original spectra with very small deviations in spectral angle map (<0.012 rad) spectral information divergence (<5.8 × 10 − 5), mean percentage relative error (MPRE) of TOARAD (<0.7 % ), and MPRE of TOA water leaving radiance (<5.8 % ). This approach possibly opens up research for application of HS analysis on MSOC recovered spectra and for optimization of sensor configurations.
Coastal eddies, frontal zones and microscale oceanographic features are now easily observable from satellite measurements of SST and Chl a. Enhancing the utility of these space-borne measurements for biological productivity, biogeochemical cycling and fisheries investigations will require novel bio-optical methods capable of providing information on the community structure, biomass and photo-physiology of phytoplankton associated on spatial scales that match these features. This study showcases high-resolution in-situ measurements of sea water hydrography (SeaBird CTD®), CDOM (WetLabs ALF®), phytoplankton functional types (PFTs, FlowCAM®), biomass (bbe Moldaenke AlgaeOnlineAnalyzer® and WetLabs ALF®) and phytoplankton photosynthetic competency (mini-FIRe) across microscale features encountered during a recent (Nov. 2014) cruise in support of NOAA's VIIRS ocean color satellite calibration and validation activities. When mapped against binned daily, Level 2 satellite images of Chl a, Kd490 and SST over the cruise period, these high-resolution in-situ data showed great correspondence with the satellite data, but more importantly allowed for identification of PFTs and water types associated with microscale features. Large assemblages of phytoplankton communities comprising of diatoms and diatom-diazotroph associations (DDAs), were found in mesohaline frontal zones. Despite their high biomass, these populations were characterized by low photosynthetic competency, indicative of a bloom at the end of its active growth possibly due to nitrogen depletion in the water. Other prominent PFTs such as Trichodesmium spp., Synechococcus spp. and cryptophytes, were also associated with specific water masses offering the promise and potential that ocean remote sensing reflectance bands when examined in the context of water types also measurable from space, could greatly enhance the utility of satellite measurements for biological oceanographic, carbon cycling and fisheries studies.
KEYWORDS: Sensors, Remote sensing, Signal to noise ratio, Atmospheric corrections, Remote sensing, Absorption, Luminescence, Near infrared, Aerosols, Short wave infrared radiation, MODIS
Selection of central wavelengths, bandwidths and the number of spectral bands of any sensor to be flown on a remote sensing satellite is important to ensure discriminability of targets and adequate signal-to-noise ratio for the retrieval of parameters. In recent years, a large number of spectral measurements over a wide variety of water types in the Arabian Sea and the Bay of Bengal have been carried out through various ship cruises. It was felt pertinent to use this precious data set to arrive at meaningful selection of spectral bands and their bandwidths of the ocean colour sensor to be flown on the forthcoming Oceansat-3 of ISRO. According to IOOCG reports and studies by Lee and Carder (2002) it is better for a sensor to have ~15 bands in the 400-800 nm range for adequate derivation of major properties (phytoplankton biomass, colored dissolved organic matter, suspended sediments, and bottom properties) in both oceanic and coastal environments from observation of water color.
In this study, ~417 hyper-spectral remote-sensing reflectance spectra (spectral range varies from ~380-800 nm) covering different water types like open, coastal, mid coastal and near coastal waters have been used to identify the suitable spectral bands for OCM-3. Central wavelengths were identified based on the results obtained from hyper-spectral underwater radiometer measurements of Rrs, HPLC pigments and spectrometer analyzed absorption spectra for all the above water types. Derivative analysis has been carried out from 1st to 5th order to identify the inflection and null points for better discrimination / identification of spectral peaks from the in situ Rrs spectra. The results showed that open ocean and coastal ocean waters has spectra peaks mostly in the blue, green region; turbid coastal waters has maximum spectral peaks in the red region. Apart from this, the spectral peaks were identified in the red region for the chlorophyll fluorescence in the open ocean and coastal waters. Based on these results 13 spectral bands were proposed in the VNIR region for the upcoming OCM-3 sensor. In order to obtain water leaving radiances from the measurements at spacecraft platform, it is necessary to do atmospheric correction we need to have spectral bands in the NIR and above regions. Hence, a set of bands 3 bands in the NIR and SWIR region were proposed for OCM-3 to address the atmospheric correction related issues.
A larger part of the heat supplied by the tropical oceans, through evaporation is utilized for development of large-scale weather systems. The knowledge of evaporation rates/Latent Heat Flux (LHF) over the ocean is essential for parameterizing Ocean–atmospheric coupled predictive models. There are several methods in estimating evaporation rates/LHF over the ocean. Among them, the prominent are (1) eddy correlation or direct method, (2) profile or gradient method and (3) bulk aerodynamic method. Here bulk-aerodynamic method is conceived, since the implementation of this method is easy and spatial and temporal coverage is very high. To calculate evaporation rate/LHF using bulk aerodynamic formulae the parameters required are Wind speed, saturated vapour pressure at sea surface temperature and vapour pressure at air temperature.
We estimated LHF using Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) data for a period of 5 years (2001-2005) during monsoon over North Indian Ocean (NIO). The LHF values found to be high in Somali region during onset phase of summer monsoon and slowly become less, though the winds become stronger. This could be due to sudden fall of SST with the onset and intense upwelling. The variations found to be larger from year to year and these variations are discussed in relation to the intensity of monsoon activity. The LHF estimates are found to be useful in studying the large-scale weather systems. The results pertaining to the study period over NIO are presented.
We examined the spatio-temporal variability of atmospheric CO2 over India and its surrounding based on Goddard Earth Observation System Chemical (GEOS-Chem) transport model, satellite and in-situ observations. The model was employed at 2x2.50 spatial resolution over the globe with 47 vertical layers between pressure levels 1006-0.01 hPa. It is driven by GEOS meteorological fields along with surface boundary fluxes and anthropogenic emissions from different sources. The model run was performed for the period 2006-2013 and the solutions at three hourly intervals were stored for the analysis. In this paper, we are discussing the seasonal and inter-annual characteristics of simulated atmospheric CO2 highlighting the uncertainties associated with input data sets in the model. There exist good coherences between model and satellite observation. Simulated CO2 shows strong seasonality near the surface and has showed decrease in its amplitude upward. Amplitudes of the seasonal and annual cycles are stronger over the northern hemisphere, especially over the land regions.
Hooghly is one of the major estuaries in Ganges, the largest and longest river in the Indian subcontinent. The Hooghly estuary is a coastal plain estuary lying approximately between 21°–23° N and 87°–89° E. We used a terrain following ocean model to study tide driven residual circulations, seasonal mean flow patterns and its energetics in the Hooghly estuary and adjacent coastal oceans on the north eastern continental shelf of India. The model is driven by tidal levels at open ocean end and winds at the air-sea interface. The sources of forcing fields for tides were from FES2012, winds from ECMWF. Harmonic analysis is carried out to compute the tidal and non-tidal components of currents and sea level from the model solutions. The de-tidal components were averaged for the entire period of simulation to describe residual and mean-seasonal circulations in the regions. We used tide-gauge, SARAL-ALTIKA along track sea level measurements to evaluate model solutions. Satellite measure Chla were used along with simulated currents to describe important features of the circulations in the region.
Timely and accurate information about land cover is an important and extensively used application of remote sensing
data. After successful launch of Landsat 8 is providing a new data source for monitoring land cover, which has the
potential to improve the earth surface features characterization. Mapping of Leaf area Index (LAI) in larger area may be
impossible when we rely on field measurements. Remote sensing data have been continuing efforts to develop different
methods to estimate LAI. In this present study, an attempt has been made to discriminate various land cover features and
empirical equation is used for retrieve biophysical parameter (LAI) for satellite NDVI data. Support vector machine
classification was performed for Muzaffarnagar district using LANDSAT 8 operational land imager data to separate out
major land cover classes (water, fallow, built up, sugarcane, orchard, dense vegetation and other crops). Ground truth
data was collected using JUNO GPS which was used in developing the spectral signatures for each classes. The LAI-NDVI
existing empirical equation is used to prepare LAI map. It is found that the LAI values in village foloda region
maximum LAI pixels in the range 3.10 and above and minimum in the range 1.0 to 1.20. It is also concluded that the
LAI values between 1.70 and 3.10 is having most of the sugarcane crop pixels at maximum vegetative growth stage. It
shows that the sugarcane crop condition in the study area was very good.
Mangroves are active carbon sequesters playing a crucial role in coastal ecosystems. In the present study, aboveground biomass (AGB) was estimated in a 5-year-old Avicennia marina plantation (approximate area ≈190 ha) of Indian Sundarbans using high-resolution satellite data in order to assess its carbon sequestration potential. The reflectance values of each band of LISS IV satellite data and the vegetation indices, viz., normalized difference vegetation index (NDVI), optimized soil adjusted vegetation index (OSAVI), and transformed difference vegetation index (TDVI), derived from the satellite data, were correlated with the AGB. OSAVI showed the strongest positive linear relationship with the AGB and hence carbon content of the stand. OSAVI was found to predict the AGB to a great extent (r2=0.72) as it is known to nullify the background soil reflectance effect added to vegetation reflectance. The total AGB of the entire plantation was estimated to be 236 metric tons having a carbon stock of 54.9 metric tons, sequestered within a time span of 5 years. Integration of this technique for monitoring and management of young mangrove plantations will give time and cost effective results.
The Resourcesat-2 (RS2), launched on April 20, 2011 is a follow-on mission to the successfully operational Resourcesat-1 (RS1). Similar to the RS1, RS2 carries 3 multispectral imagers in its platform: the Advanced Wide-
Field Sensor (AWiFS), the Linear Imaging Self-Scanner (LISS 3) and the high-resolution multi-spectral scanner
LISS-4. This study focuses on assessment of the radiometric calibration stability of RS2 AWiFS sensor by comparing near-simultaneous measurements of Terra MODIS acquired over CEOS reference standard targets. The AWiFS sensor operates four distinct spectral bands: B2 (0.52-0.59 μm), B3 (0.63-0.69 μm), B4 (0.77-0.86 μm) and B5 (1.55-1.7 μm) with a spatial resolution of 56 m. Only those bands of the Terra MODIS spectrally matching to AWiFS bands are compared after basic corrections for variations due to the sun and satellite angles with reference to scene center and the atmospheric transmittance on the given day of acquisition. Synchronous acquisitions of these
sensors over the desert regions in Libya, Algeria and Egypt at CEOS recommended geographic coordinates were
acquired and processed to compare the top-of-atmosphere (TOA) reflectance from both sensors. Preliminary results and future efforts are also discussed in this paper.
Monitoring and management of land use plays an important role in the economic development of agriculture regions around the world. In this regard, field boundary extraction for agriculture land parcels is crucial for further analysis and mapping. An effective image analysis needs to perform this task by automatically extracting the features with minimum operator efforts. Many researchers have attempted land use/land cover classification using IRS P6 LISS IV data. However little emphasis has been given to agriculture field boundary extraction. This paper explores the potential of IRS P-6 LISS IV dataset for agriculture field boundary extraction. The segmentation of field areas based on the tonal and textural gradients of the imagery is carried out. The segmented regions were classified to derive preliminary field boundaries. Finally, the derived field boundaries are geometrically refined using snakes. The use of snakes resulted in marked improvement in preliminary results. It was observed that traditional snakes can be effectively applied on single closed boundary at a time, which makes it suitable for single target detection. An attempt has been made in this study to develop looping snakes which can deal with multiple boundaries as will be the case with objects like agriculture fields.
A comparative study between two approaches of subpixel classification, based on fuzzy set theory and statistical learning has been carried out. The fuzzy set classifiers investigated in this study are Fuzzy c-Means (FCM) and Possibilistic c-Means (PCM) in supervised modes. Further, Support Vector Machines (SVMs) have been used in this study for density estimation as a statistical learning subpixel classifier and Mean Field (MF) method has been used for easy and efficient learning procedure for the SVM. The three algorithms FCM, PCM and SVMs were evaluated in subpixel classification mode and accuracy assessment has been carried out using Fuzzy Error Matrix (FERM). Test on the two sub sets of LISS-III multi-spectral image from Resourcesat -1, (IRS-P6) satellite, indicates that density estimation based on SVM approach is consistent with different data sets and out performs both FCM as well as PCM approach.
Wheat is an important food crop of the country. Its productivity lies in a very wide
range due to diverse bio-physical and socio-economic conditions in the growing regions.
Crop cutting and sample surveys are time consuming as well tedious, and procedure of
forecast is delayed. CAPE methodology, which uses remote sensing, ground truth and
prevailing weather, has been very successful, but empirical in nature. In a joint IARI-SAC
Research Programme, possibility of linking the dynamic wheat growth model with the
remote sensing input and other relational database layers was tried. Use of WTGROWS, a
wheat growth model developed at IARI, with the remote sensing and relational databases
is dynamic and can be updated whenever weather, acreage and fertilizer and other inputs
are received. National wheat yield forecast was done for three seasons on meteorological
sub-division scale by using WTGROWS, relational database layers and satellite image.
WTGROWS was run for historic weather dataset (last 25 years), with the relational
database inputs through their associated growth rates and compared with the productivity
trends of the met-subdivision. Calibration factor, for each met-subdivision, were obtained
to capture the other biotic and abiotic stresses and subsequently used to bring down the
yields at each sub-division to realistic scale. The satellite image was used to compute the
acreage with wheat in each sub-division. Meteorological data for each-subdivision was
obtained from IMD (weekly basis). WTGROWS was run with actual weather data obtained upto a given time, and weather normals use for subsequent period, and the forecast was
prepared. This was updated on weekly basis, and the methodology could forecast the
wheat yield well in advance with a great accuracy. This procedure shows the pathway for
Crop Growth Monitoring System (CGMS) for the country, to be used for land use planning
and agri-production estimates, which although looks difficult for diverse agro-ecologies and
wide range of bio-physical and socio-economic characters contributing to differential
productivity trends.
A study was undertaken to validate the Wheat Growth Simulator (WTGROWS) in the farmers' fields of Alipur Block of Delhi and linking satellite derived vegetation index with the simulation model to estimate the wheat yield. Date of sowing, management practices and cultivars varied widely among the study sites. Leaf area index (LAI), phenological development and agronomic management (fertilizers and irrigation) were monitored at regular intervals for the 25 field sites selected in the study area. Above ground biomass and grain yield were recorded at harvest. Using the parameters derived for these sites, WTGROWS was run for each of the individual 25 sites. Crop phenology, temporal course of LAI and grain yield of each site was compared with the actual observations. The simulated and actual LAI temporal profile matched well for sites with different dates of sowing, excepting larger deviation noticed in the later stages of the crop growth. The simulated pre-anthesis duration and total above ground biomass were also correlated well with the observed values being mostly within ±15%. There were large discrepancies in simulated and observed grain yield. A satellite image near anthesis of IRS 1D LISS-3 was acquired for the study area. The sites were identified on the image and their vegetation indices were derived. Average grey value in Infrared (IR) and Red (R) band, Ratio Vegetation Index (RVI), Soil Adjusted Vegetation Index (SAVI) and Normalized Difference Vegetation Index (NDVI) were giving significant relation with measured LAI of 5th February which corresponded to crop anthesis stage. The relation between vegetation indices and LAI was logarithmic in nature. This logarithmic relation was incorporated into the WTGROWS to force the LAI to the equation-derived value at particular growth stage and model yield was computed and compared with actual observations.
KEYWORDS: Soil science, Decision support systems, Geographic information systems, Remote sensing, Data modeling, Carbon, Databases, Human-machine interfaces, Climatology, Water
Spatial databases of natural resources are very much essential to ensure enhanced productivity by conserving
soil and water and to maintain ecological integrity of any region. Integration of various thematic layers prepared from
high resolution data and detailed field survey would be preferred for grass root level planning (Panchayat) aimed to
realize the potential of production system on a sustained basis. In this study, a detailed spatial data base was created for
part of Kasaragod dist., Kerala, India. Detailed soil survey was carried out using cadastral map and registered over high
resolution satellite data (IRS LISS-IV) which helped to identify problems and potentials of the area. Nearly 600 ha of
land were found to be at higher erosion risk category out of ten soil series identified in the study area. Remote sensing
data was used to prepare land use/land cover map and coconut (53%) followed by mixed vegetation type (16%) were
found to be dominant. Soil site suitability assessment for major crops of the area was carried out and crossed with
present land use to get the mismatch in land use/land utilization type. Alternate land use plan was prepared considering
the potentials and problems of various available resources. Decision Support System (DSS) along with user interface is
developed to support decision and extract relevant information. As organic carbon is one of the most important
indicators of soil fertility C stock in the present and proposed land use was also estimated to understand the
environmental significance.
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