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A New Differential Optical Absorption Spectroscopy Instrument to Study Atmospheric Chemistry from a High-Altitude Unmanned Aircraft.

Authors :
Stutz, Jochen
Werner, Bodo
Spolaor, Max
Scalone, Lisa
Festa, James
Tsai, Catalina
Cheung, Ross
Colosimo, Santo~F.
Tricoli, Ugo
Raecke, Rasmus
Hossaini, Ryan
Chipperfield, Martyn~P.
Wuhu Feng
Ru-Shan Gao
Hintsa, Eric~J.
Elkins, James~W.
Moore, Fred~L.
Daube, Bruce
Pittman, Jasna
Wofsy, Steven
Source :
Atmospheric Measurement Techniques Discussions; 2016, p1-48, 48p
Publication Year :
2016

Abstract

Observations of atmospheric trace gases in the tropical upper troposphere (UT), tropical tropopause layer (TTL) and lower stratosphere (LS) require dedicated measurement platforms and instrumentation. Here we present a new limb-scanning Differential Optical Absorption Spectroscopy (DOAS) instrument developed for NASA's Global Hawk unmanned aerial system (GH) during the Airborne Tropical TRopopause EXperiment (ATTREX). The mini-DOAS system is designed for automatic operation under unpressurized and unheated conditions at 14-18 km altitude, collecting scattered sunlight in three wavelength windows: UV (301-387 nm), visible (410-525 nm) and near infrared (900-1700 nm). A telescope scanning unit allows selection of a viewing angle around the limb, as well as real-time correction of the aircraft pitch. Due to the high altitude, solar reference spectra are measured using diffusors and direct sunlight. The DOAS approach allows retrieval of slant column densities (SCD) of O<subscript>3</subscript>, O<subscript>4</subscript>, NO<subscript>2</subscript>, and BrO with relative errors similar to other aircraft DOAS systems. Radiative transfer considerations show that the retrieval of trace gas mixing ratios from the observed SCD based on O<subscript>4</subscript> observations, the most common approach for DOAS measurements, is inadequate for high-altitude observations, due to frequent presence of low altitude clouds. A newly developed technique that constrains the radiative transfer (RT) by comparing in-situ and DOAS O<subscript>3</subscript> observations overcomes this issue. Extensive sensitivity calculations show that the novel O<subscript>3</subscript>-scaling technique allows the retrieval of BrO and NO<subscript>2</subscript> mixing ratios at high accuracies of 0.3-0.6 ppt and 15 ppt, respectively. The BrO and NO<subscript>2</subscript> mixing ratios and vertical profiles observed during ATTREX thus provide new insights into ozone and halogen chemistry in the UT, TTL, and LS. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
18678610
Database :
Complementary Index
Journal :
Atmospheric Measurement Techniques Discussions
Publication Type :
Academic Journal
Accession number :
119961815
Full Text :
https://doi.org/10.5194/amt-2016-251