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Open AccessJournal ArticleDOI

The optical and physical properties of atmospheric aerosols over the Indian Antarctic stations during southern hemispheric summer of the International Polar Year 2007–2008

TLDR
In this article, the authors examined the properties of background aerosols and their dependence on meteorological, geographical and human influence using measured spectral aerosol optical depth (AOD), total mass concentration (M T ) and derived number size distribution (NSD) over two distinct coastal locations of Antarctica; Maitri (70° S, 12° E, 123 m m.s.l.
Abstract
. The properties of background aerosols and their dependence on meteorological, geographical and human influence are examined using measured spectral aerosol optical depth (AOD), total mass concentration ( M T ) and derived number size distribution (NSD) over two distinct coastal locations of Antarctica; Maitri (70° S, 12° E, 123 m m.s.l.) and Larsemann Hills (LH; 69° S, 77° E, 48 m m.s.l.) during southern hemispheric summer of 2007–2008 as a part of the 27th Indian Scientific Expedition to Antarctica (ISEA) during International Polar Year (IPY). Our investigations showed comparable values for the mean columnar AOD at 500 nm over Maitri (0.034±0.005) and LH (0.032±0.006) indicating good spatial homogeneity in the columnar aerosol properties over the coastal Antarctica. Estimation of Angstrom exponent α showed accumulation mode dominance at Maitri (α~1.2±0.3) and coarse mode dominance at LH (0.7±0.2). On the other hand, mass concentration ( M T ) of ambient aerosols showed relatively high values (≈8.25±2.87 μg m −3 ) at Maitri in comparison to LH (6.03±1.33 μg m −3 ).

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Journal ArticleDOI

High altitude (∼4520 m amsl) measurements of black carbon aerosols over western trans‐Himalayas: Seasonal heterogeneity and source apportionment

TL;DR: The first ever, year-round measurements of aerosol black carbon (BC) over the western part of trans- Himalayas are reported from Hanle (∼4520 m above mean sea level) as discussed by the authors.
Journal ArticleDOI

A New Satellite-Based Global Climatology of Dust Aerosol Optical Depth

TL;DR: In this paper, two nearly global observation data sets were used to identify the largest contributor to global aerosol burden, by mass, from the ocean surface, particularly over the ocean, where long-term observational records of dust are limited.
Journal ArticleDOI

Aerosol characteristics at the three poles of the Earth as characterized by Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations

TL;DR: In this article, the authors investigated the aerosol optical properties over the Arctic, Antarctic and Tibetan Plateau (TP), using 13 years of CALIPSO (Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations) L3 data, and the back trajectories for air masses were also simulated using the Hybrid Single Particle Lagrangian Integrated trajectory (HYSPLIT) model.
Journal ArticleDOI

Black carbon aerosol and its radiative impact at a high-altitude remote site on the southeastern Tibet Plateau

TL;DR: In this article, the authors measured aerosol black carbon (BC) with an Aethalometer™ at Lulang, a high-altitude station in southeastern Tibetan Plateau (TP), from July 2008 to August 2009, indicating a significant BC burden even at free tropospheric altitudes.
References
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Journal ArticleDOI

Soot climate forcing via snow and ice albedos

TL;DR: Reducing soot emissions, thus restoring snow albedos to pristine high values, would have the double benefit of reducing global warming and raising the global temperature level at which dangerous anthropogenic interference occurs.
Journal ArticleDOI

The parameters of atmospheric turbidity

Anders Ångström
- 01 Feb 1964 - 
TL;DR: In this paper, a method first suggested by M. Herovanu (1959) is used for deriving the named turbidity parameters in adherence to a procedure described by the present author in a previous paper in this journal.
Journal ArticleDOI

Marine aerosol, sea-salt, and the marine sulphur cycle: a short review

TL;DR: A short review of the marine aerosol size distribution and the contribution of sea-salt to this distribution is presented in this paper, where the potential role of sea salt in the marine boundary layer sulphur cycle is highlighted.
Journal ArticleDOI

Marine aerosols: A review

TL;DR: The background aerosol in the boundary layer over the remote oceans is not aged continental aerosol but, rather, is largely of marine origin this article, and the principal gas-toparticle conversion mechanisms are particle formation by homogeneous nucleation of lowvolatility gas-phase reaction products, condensation of these products on existing particles, and SO2-to-sulfate conversion in cloud droplets.
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