2008
DOI: 10.1007/s12040-008-0017-y
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Aerosol characteristics at a remote island: Minicoy in southern Arabian Sea

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Cited by 19 publications
(8 citation statements)
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“…5c) is consistent with ground-based observations. The role of low AOD over the Arabian Sea and Bay of Bengal in producing the latitudinal and longitudinal variation in AOD observed in our study is corroborated by the studies of Vinoj et al (2008) and Naseema Beegum et al (2012). Vi- In order to further explore the model-satellite comparison, we examined the correlation coefficients of some of the models: IPSL-CM5A-MR (Dufresne et al, 2013), CSIRO-BOM-ACCESS1.0 (Bi et al, 2013), NOAA-GFDL-ESM2M, NOAA-GFDL-ESM2G (Dunne et al, 2012), MIROC-MIROC5 (Watanabe et al, 2010), MRI-CGCM3 (Yukimoto et al, 2012), NCC-NorESM1-M , NCC-NorESM1-ME (Tjiputra et al, 2013) over selected regions (Fig.…”
Section: Cmip5supporting
confidence: 90%
“…5c) is consistent with ground-based observations. The role of low AOD over the Arabian Sea and Bay of Bengal in producing the latitudinal and longitudinal variation in AOD observed in our study is corroborated by the studies of Vinoj et al (2008) and Naseema Beegum et al (2012). Vi- In order to further explore the model-satellite comparison, we examined the correlation coefficients of some of the models: IPSL-CM5A-MR (Dufresne et al, 2013), CSIRO-BOM-ACCESS1.0 (Bi et al, 2013), NOAA-GFDL-ESM2M, NOAA-GFDL-ESM2G (Dunne et al, 2012), MIROC-MIROC5 (Watanabe et al, 2010), MRI-CGCM3 (Yukimoto et al, 2012), NCC-NorESM1-M , NCC-NorESM1-ME (Tjiputra et al, 2013) over selected regions (Fig.…”
Section: Cmip5supporting
confidence: 90%
“…Enhanced production of maritime aerosols by strong surface wind (Figure 4) also contributes to the observed increase of AOD over the Arabian Sea in this season along with dust, thus showing low AE (<0.6) compared to over the land. Ground‐based measurements of spectral AOD by multiwavelength radiometer at Minicoy (Figure 1) also show AE of ∼0.4 during this season [ Vinoj et al , 2008]. Unfortunately, data from Port Blair in the Bay of Bengal (Figure 1) are not available in the literature for comparison in this season.…”
Section: Climatology Of Aerosol Propertiesmentioning
confidence: 99%
“…By combining MODIS‐derived AOD and NCEP‐derived wind data, Satheesh et al [2006d] have shown that during the monsoon season, the relative contribution of maritime aerosols to the AOD over the northern Arabian Sea is lower than that over the southern Arabian Sea. The air mass to the northern Arabian Sea has been found to come from west Asia and Africa [ Satheesh et al , 2006d], whereas the air mass to the southern Arabian Sea comes from the open oceans [ Vinoj et al , 2008]. We have also looked into the spatial gradient of the absorbing aerosol index (AAI) over the Arabian Sea (not shown here) from Total Ozone Mapping Spectrometer (TOMS, for data up to the year 2005) and Ozone Monitoring Instrument (OMI, after the year 2005).…”
Section: Climatology Of Aerosol Propertiesmentioning
confidence: 99%
“…In recent years, the groundbased network of aerosol measurements has expanded in the country as part of the Aerosol Radiative Forcing over India (ARFI) project under Indian Space Research Organization's Geosphere Biosphere Programme (Kompalli et al, 2010), which has been extensively used to quantify aerosol direct radiative forcing at several places (e.g. Babu et al, 2002;Moorthy et al, 2005;Vinoj et al, 2008). Satellite data were also analyzed to understand the space-time distribution of aerosols in the subcontinent (Di Girolamo et al, 2004;Jethva et al, 2005;Ramachandran and Cherian, 2008;Dey and Di Girolamo, 2010).…”
Section: Introductionmentioning
confidence: 99%