4.7 Article

Case study of stratospheric intrusion above Hampton, Virginia: Lidar-observation and modeling analysis

Journal

ATMOSPHERIC ENVIRONMENT
Volume 259, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.atmosenv.2021.118498

Keywords

Lidar; Ozone; Stratospheric intrusion; Model 2010 MSC; 00-01; 99-00

Funding

  1. NASA Tropospheric Composition Program
  2. LMOL
  3. NASA Modeling, Analysis and Prediction (MAP) program
  4. NOAA Climate Program Office, Atmospheric Chemistry, Carbon Cycle, and Climate (AC4) Program
  5. NASA

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A study detected a stratospheric intrusion event above Hampton, Virginia using NASA's LMOL and MPL instruments, with the GEOS-CF model confirming the stratospheric origin of the air mass. The research showed that particulate observations could potentially be used as a signature of stratospheric intrusions and that the LMOL system has the capability to detect such events.
On 2019-02-14, at 1:00 UTC, a large increase of ozone density at 8 km altitude was detected above Hampton, Virginia using the NASA Langley Mobile Ozone Lidar, LMOL. Ozone levels above 70 ppbv were observed down to an altitude of 4.5 km up to 5 h after the start of the event. The NASA GEOS Composition Forecast (GEOS-CF) model was used to investigate the hypothesis of a stratospheric intrusion (SI). The agreement between the model and the observations confirmed the stratospheric origin of the airmass and highlighted the capabilities of GEOS-CF to simulate intrusions. In parallel, MicroPulse Lidar (MPL) observations indicated that depolarizing particulates high in the troposphere showed downward motions linked to the intrusion. Since these particulates are linked to cirrus clouds, it is hypothesised that the SI led to an ice-virga effect. This might suggest that particulate observations can exhibit patterns of stratospheric intrusions and can be used, in certain cases, as a signature of the events. These particulates, likely ice crystals, have opposite distribution gradients compared to O-3 at their interface which could be explained by a non-mixing of stratospheric and tropospheric air-masses as well as destruction of O-3 by ice crystal-induced processes. Model-data comparison shows that if that latter effect exists, it has small consequences for the observed case. This work shows the capabilities of the LMOL system to detect SI and to validate the vertical and temporal modeling of SI by GEOS-CF, as well as showing that signatures of SI could be detected by MPL.

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