References

ACPD

Atmospheric Chemistry and Physics Discussions

ACPD

Atmos. Chem. Phys. Discuss.

1680-7375

Göttingen, Germany

10.5194/acpd-11-4229-2011

Continuous observations of synoptic-scale dust transport at the Nepal Climate Observatory-Pyramid (5079 m a.s.l.) in the Himalayas

Duchi

¹ ⁷ Cristofanelli

¹ Marinoni

¹ Laj

² Marcq

² Villani

² Sellegri

³ Angelini

⁴ Calzolari

¹ Gobbi

G. P.

⁴ Verza

G. P.

⁵ Vuillermoz

⁵ Sapkota

⁶ Bonasoni

¹ ⁵

CNR-Institute of Atmospheric Sciences and Climate, Bologna, Italy

Laboratoire de Glaciologie et Géophysique de l'Environnement, Université Grenoble 1-CNRS, Grenoble, France

Laboratoire de Météorologie Physique, CNRS – Université Blaise Pascal, Aubière, France

CNR-Institute of Atmospheric Sciences and Climate, Rome, Italy

Ev-K2-CNR Committee, Bergamo, Italy

Department of Environment Science and Engineering, Kathmandu University, Dhulikhel, Nepal

Science and Technology Faculty, Urbino University, Urbino, Italy

04 02 2011

11 2 4229 4261

2011

This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit https://creativecommons.org/licenses/by/3.0/

This article is available from https://acp.copernicus.org/preprints/11/4229/2011/acpd-11-4229-2011.html

The full text article is available as a PDF file from https://acp.copernicus.org/preprints/11/4229/2011/acpd-11-4229-2011.pdf

This study presents two years of continuous observations of physical aerosol properties at the GAW-WMO global station "Nepal Climate Observatory – Pyramid" (NCO-P, 27°57' N, 86°48' E), sited at 5079 m a.s.l. in the high Himalayan Khumbu Valley (Nepal). Measurements of aerosol number size distribution, aerosol optical depth (AOD) and single scattering albedo (SSA) are analysed from March 2006 to February 2008. By studying the temporal variations of coarse (1 μm < Dp ≤ 10 μm) particle number concentration, 53 mineral Dust Transport Events (DTEs) are identified, accounting for 22.2% of the analysed data-set. Such events occurred prevalently during pre-monsoon (for 30.6% of the period) and winter (22.1%) seasons. However, uncommon cases of mineral dust transport are observed even during the monsoon season. The main sources of mineral dust reaching NCO-P are identified in the arid regions not far from the measurement site, i.e. from Tibetan Plateau, and Lot-Thar deserts, which account for 52% of the dust transport days. Moreover, a non-negligible contribution can be attributed to the Arabian Peninsula (17%) and the Indo-Gangetic Plains (16%), as indicated by three dimensional (3-D) back-trajectory analyses performed with LAGRANTO model. The observed DTEs lead to significant enhancements in the coarse aerosol number concentration (+513%) and coarse aerosol mass (+655%), as compared with average values observed in "dust-free" conditions ( 0.05 ± 0.11 cm−3 and 3.4 ± 3.7 μg m−3, respectively). During DTEs, SSA is higher (0.84–0.89) than on "dust-free" days (0.75–0.83), confirming the importance of this class of events as a driver of the radiative features of the regional Himalayan climate. Considering the dust events, a significant seasonal AOD increase (+37.5%) is observed in the post-monsoon, whereas lower increase (less than +11.1%) characterises the pre-monsoon and winter seasons confirming the influence of synoptic-scale mineral dust transports on the aerosol optical properties observed at NCO-P.

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