An analysis of the cloud environment over the Ross Sea and Ross Ice Shelf using CloudSat/CALIPSO satellite observations: the importance of synoptic forcing

<p>We use the 2B-GEOPROF-LIDAR R04 (2BGL4) and R05 (2BGL5) products and the 2B-CLDCLASS-LIDAR R04 (2BCL4) product, all generated by combining CloudSat radar and CALIPSO lidar satellite measurements with auxiliary data, to examine the vertical distribution of cloud occurrence around the Ross...

Full description

Bibliographic Details
Main Authors: B. Jolly, P. Kuma, A. McDonald, S. Parsons
Format: Article
Language:English
Published: Copernicus Publications 2018-07-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/18/9723/2018/acp-18-9723-2018.pdf
id doaj-76673004818f4f3a89f0deb6e628f72b
record_format Article
spelling doaj-76673004818f4f3a89f0deb6e628f72b2020-11-24T20:50:18ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242018-07-01189723973910.5194/acp-18-9723-2018An analysis of the cloud environment over the Ross Sea and Ross Ice Shelf using CloudSat/CALIPSO satellite observations: the importance of synoptic forcingB. Jolly0P. Kuma1A. McDonald2S. Parsons3Landcare Research, Lincoln, New ZealandDepartment of Physics and Astronomy, University of Canterbury, Christchurch, New ZealandDepartment of Physics and Astronomy, University of Canterbury, Christchurch, New ZealandDepartment of Physics and Astronomy, University of Canterbury, Christchurch, New Zealand<p>We use the 2B-GEOPROF-LIDAR R04 (2BGL4) and R05 (2BGL5) products and the 2B-CLDCLASS-LIDAR R04 (2BCL4) product, all generated by combining CloudSat radar and CALIPSO lidar satellite measurements with auxiliary data, to examine the vertical distribution of cloud occurrence around the Ross Ice Shelf (RIS) and Ross Sea region. We find that the 2BGL4 product, used in previous studies in this region, displays a discontinuity at 8.2 km which is not observable in the other products. This artefact appears to correspond to a change in the horizontal and vertical resolution of the CALIPSO dataset used above this level. We then use the 2BCL4 product to examine the vertical distribution of cloud occurrence, phase, and type over the RIS and Ross Sea. In particular we examine how synoptic conditions in the region, derived using a previously developed synoptic classification, impact the cloud environment and the contrasting response in the two regions. We observe large differences between the cloud occurrence as a function of altitude for synoptic regimes relative to those for seasonal variations. A stronger variation in the occurrence of clear skies and multi-layer cloud and in all cloud type occurrences over both the Ross Sea and RIS is associated more with synoptic type than seasonal composites. In addition, anomalies from the mean joint histogram of cloud top height against thickness display significant differences over the Ross Sea and RIS sectors as a function of synoptic regime, but are near identical over these two regions when a seasonal analysis is completed. However, the frequency of particular phases of cloud, notably mixed phase and water, is much more strongly modulated by seasonal than synoptic regime compositing, which suggests that temperature is still the most important control on cloud phase in the region.</p>https://www.atmos-chem-phys.net/18/9723/2018/acp-18-9723-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author B. Jolly
P. Kuma
A. McDonald
S. Parsons
spellingShingle B. Jolly
P. Kuma
A. McDonald
S. Parsons
An analysis of the cloud environment over the Ross Sea and Ross Ice Shelf using CloudSat/CALIPSO satellite observations: the importance of synoptic forcing
Atmospheric Chemistry and Physics
author_facet B. Jolly
P. Kuma
A. McDonald
S. Parsons
author_sort B. Jolly
title An analysis of the cloud environment over the Ross Sea and Ross Ice Shelf using CloudSat/CALIPSO satellite observations: the importance of synoptic forcing
title_short An analysis of the cloud environment over the Ross Sea and Ross Ice Shelf using CloudSat/CALIPSO satellite observations: the importance of synoptic forcing
title_full An analysis of the cloud environment over the Ross Sea and Ross Ice Shelf using CloudSat/CALIPSO satellite observations: the importance of synoptic forcing
title_fullStr An analysis of the cloud environment over the Ross Sea and Ross Ice Shelf using CloudSat/CALIPSO satellite observations: the importance of synoptic forcing
title_full_unstemmed An analysis of the cloud environment over the Ross Sea and Ross Ice Shelf using CloudSat/CALIPSO satellite observations: the importance of synoptic forcing
title_sort analysis of the cloud environment over the ross sea and ross ice shelf using cloudsat/calipso satellite observations: the importance of synoptic forcing
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2018-07-01
description <p>We use the 2B-GEOPROF-LIDAR R04 (2BGL4) and R05 (2BGL5) products and the 2B-CLDCLASS-LIDAR R04 (2BCL4) product, all generated by combining CloudSat radar and CALIPSO lidar satellite measurements with auxiliary data, to examine the vertical distribution of cloud occurrence around the Ross Ice Shelf (RIS) and Ross Sea region. We find that the 2BGL4 product, used in previous studies in this region, displays a discontinuity at 8.2 km which is not observable in the other products. This artefact appears to correspond to a change in the horizontal and vertical resolution of the CALIPSO dataset used above this level. We then use the 2BCL4 product to examine the vertical distribution of cloud occurrence, phase, and type over the RIS and Ross Sea. In particular we examine how synoptic conditions in the region, derived using a previously developed synoptic classification, impact the cloud environment and the contrasting response in the two regions. We observe large differences between the cloud occurrence as a function of altitude for synoptic regimes relative to those for seasonal variations. A stronger variation in the occurrence of clear skies and multi-layer cloud and in all cloud type occurrences over both the Ross Sea and RIS is associated more with synoptic type than seasonal composites. In addition, anomalies from the mean joint histogram of cloud top height against thickness display significant differences over the Ross Sea and RIS sectors as a function of synoptic regime, but are near identical over these two regions when a seasonal analysis is completed. However, the frequency of particular phases of cloud, notably mixed phase and water, is much more strongly modulated by seasonal than synoptic regime compositing, which suggests that temperature is still the most important control on cloud phase in the region.</p>
url https://www.atmos-chem-phys.net/18/9723/2018/acp-18-9723-2018.pdf
work_keys_str_mv AT bjolly ananalysisofthecloudenvironmentovertherossseaandrossiceshelfusingcloudsatcalipsosatelliteobservationstheimportanceofsynopticforcing
AT pkuma ananalysisofthecloudenvironmentovertherossseaandrossiceshelfusingcloudsatcalipsosatelliteobservationstheimportanceofsynopticforcing
AT amcdonald ananalysisofthecloudenvironmentovertherossseaandrossiceshelfusingcloudsatcalipsosatelliteobservationstheimportanceofsynopticforcing
AT sparsons ananalysisofthecloudenvironmentovertherossseaandrossiceshelfusingcloudsatcalipsosatelliteobservationstheimportanceofsynopticforcing
AT bjolly analysisofthecloudenvironmentovertherossseaandrossiceshelfusingcloudsatcalipsosatelliteobservationstheimportanceofsynopticforcing
AT pkuma analysisofthecloudenvironmentovertherossseaandrossiceshelfusingcloudsatcalipsosatelliteobservationstheimportanceofsynopticforcing
AT amcdonald analysisofthecloudenvironmentovertherossseaandrossiceshelfusingcloudsatcalipsosatelliteobservationstheimportanceofsynopticforcing
AT sparsons analysisofthecloudenvironmentovertherossseaandrossiceshelfusingcloudsatcalipsosatelliteobservationstheimportanceofsynopticforcing
_version_ 1716804113949261824