Satellite observation of stratospheric intrusions and ozone transport using CrIS on SNPP

Clouds in the tropics have an important role in the energy budget, atmospheric circulation, humidity, and composition of the tropical-to-global upper-troposphere–lower-stratosphere. Due to its non-sun-synchronous orbit, the Cloud–Aerosol Transport System (CATS) onboard the International Space Station (ISS) provided novel information on clouds from space in terms of overpass time in the period of 2015–2017. In this paper, we provide a seasonally resolved comparison of CATS characterization of high clouds (between 13 and 18 km altitude) in the tropics with well-established CALIPSO (Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observation) data, both in terms of clouds’ occurrence and cloud optical properties (optical depth). Despite the fact that cloud statistics for CATS and CALIOP are generated using intrinsically different local overpass times, the characterization of high clouds occurrence and optical properties in the tropics with the two instruments is very similar. Observations from CATS underestimate clouds occurrence (up to 80%, at 18 km) and overestimate the occurrence of very thick clouds (up to 100% for optically very thick clouds, at 18 km) at higher altitudes. Thus, the description of stratospheric overshoots with CATS and CALIOP might be different. While this study hints at the consistency of CATS and CALIOP clouds characterizaton, the small differences highlighted in this work should be taken into account when using CATS for estimating cloud properties and their variability in the tropics.

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Global Aerosol Classification Based on Aerosol Robotic Network (AERONET) and Satellite Observation

Remote Sensing ◽

10.3390/rs13061114 ◽

2021 ◽

Vol 13 (6) ◽

pp. 1114

Author(s):

Jianyu Lin ◽

Yu Zheng ◽

Xinyong Shen ◽

Lizhu Xing ◽

Huizheng Che

Keyword(s):

Radiative Forcing ◽

Temporal Distribution ◽

Satellite Observation ◽

Western Africa ◽

Deep Blue ◽

Sensing Technology ◽

Aerosol Classification ◽

Linear Depolarization Ratio ◽

Absorbing Aerosols ◽

Single Scatter

The particle linear depolarization ratio (PLDR) and single scatter albedo (SSA) in 1020 nm from the Aerosol Robotic Network (AERONET) level 2.0 dataset was utilized among 52 stations to identify dust and dust dominated aerosols (DD), pollution dominated mixture (PDM), strongly absorbing aerosols (SA) and weakly absorbing aerosols (WA), investigate their spatial and temporal distribution, net radiative forcing and radiative forcing efficiency in global range, and further compare with VIIRS Deep Blue Production. The conclusion about net radiative forcing suggests that the high values of radiative forcing from dust and dust dominated aerosols, pollution dominated mixture both mainly come from western Africa. Strongly absorbing aerosols in South Africa and India contribute greatly to the net radiative forcing and the regions with relative high values of weakly absorbing aerosols are mainly located at East Asia and India. Lastly, the observation of VIIRS Deep Blue satellite monthly averaged products depicts the characteristics about spatial distribution of four kinds of aerosol well, the result from ground-based observation presents great significant to validate the measurements from remote sensing technology.

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Springtime high surface ozone events over the western United States: Quantifying the role of stratospheric intrusions

Journal of Geophysical Research Atmospheres ◽

10.1029/2012jd018151 ◽

2012 ◽

Vol 117 (D21) ◽

pp. n/a-n/a ◽

Cited By ~ 168

Author(s):

Meiyun Lin ◽

Arlene M. Fiore ◽

Owen R. Cooper ◽

Larry W. Horowitz ◽

Andrew O. Langford ◽

...

Keyword(s):

United States ◽

Surface Ozone ◽

High Surface ◽

Western United States ◽

Stratospheric Intrusions

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Ozone Transport Assessment Group: recommended control strategies

IECEC 96. Proceedings of the 31st Intersociety Energy Conversion Engineering Conference ◽

10.1109/iecec.1996.553564 ◽

2002 ◽

Author(s):

S.L. Gerritson

Keyword(s):

Control Strategies ◽

Ozone Transport

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Eddy meridional ozone transport in Antarctica in August–October 1998 and 2002

International Journal of Remote Sensing ◽

10.1080/01431160500076483 ◽

2005 ◽

Vol 26 (16) ◽

pp. 3441-3447

Author(s):

P. N. Vargin

Keyword(s):

Ozone Transport

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Effects of atmospheric dynamics and aerosols on the fraction of supercooled water clouds

Atmospheric Chemistry and Physics ◽

10.5194/acp-17-1847-2017 ◽

2017 ◽

Vol 17 (3) ◽

pp. 1847-1863 ◽

Cited By ~ 30

Author(s):

Jiming Li ◽

Qiaoyi Lv ◽

Min Zhang ◽

Tianhe Wang ◽

Kazuaki Kawamoto ◽

...

Keyword(s):

Relative Humidity ◽

Vertical Velocity ◽

Meteorological Parameters ◽

Temporal Correlation ◽

Supercooled Liquid ◽

Satellite Observation ◽

Static Stability ◽

Global Scale ◽

Atmospheric Dynamics ◽

Horizontal Wind

Abstract. Based on 8 years of (January 2008–December 2015) cloud phase information from the GCM-Oriented Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Cloud Product (GOCCP), aerosol products from CALIPSO and meteorological parameters from the ERA-Interim products, the present study investigates the effects of atmospheric dynamics on the supercooled liquid cloud fraction (SCF) during nighttime under different aerosol loadings at global scale to better understand the conditions of supercooled liquid water gradually transforming to ice phase. Statistical results indicate that aerosols' effect on nucleation cannot fully explain all SCF changes, especially in those regions where aerosols' effect on nucleation is not a first-order influence (e.g., due to low ice nuclei aerosol frequency). By performing the temporal and spatial correlations between SCFs and different meteorological factors, this study presents specifically the relationship between SCF and different meteorological parameters under different aerosol loadings on a global scale. We find that the SCFs almost decrease with increasing of aerosol loading, and the SCF variation is closely related to the meteorological parameters but their temporal relationship is not stable and varies with the different regions, seasons and isotherm levels. Obviously negative temporal correlations between SCFs versus vertical velocity and relative humidity indicate that the higher vertical velocity and relative humidity the smaller SCFs. However, the patterns of temporal correlation for lower-tropospheric static stability, skin temperature and horizontal wind are relatively more complex than those of vertical velocity and humidity. For example, their close correlations are predominantly located in middle and high latitudes and vary with latitude or surface type. Although these statistical correlations have not been used to establish a certain causal relationship, our results may provide a unique point of view on the phase change of mixed-phase cloud and have potential implications for further improving the parameterization of the cloud phase and determining the climate feedbacks.

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