Identifying a Leading Predictor of Arctic Stratospheric Ozone for April Precipitation in Eastern North America

An analysis of the relationship between changes in Arctic stratospheric ozone (ASO) and precipitation in eastern North America (38°–54°N, 65°–87°W; PENA) was performed using observational and reanalysis data coupled with the Whole Atmosphere Community Climate Model version 4 (WACCM4). We found that...

Full description

Bibliographic Details
Published in:Remote Sensing
Main Authors: Xuan Ma, Fei Xie, Xiaosong Chen, Lei Wang, Guanyu Yang
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/rs14195040
id ftmdpi:oai:mdpi.com:/2072-4292/14/19/5040/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2072-4292/14/19/5040/ 2023-08-20T04:04:06+02:00 Identifying a Leading Predictor of Arctic Stratospheric Ozone for April Precipitation in Eastern North America Xuan Ma Fei Xie Xiaosong Chen Lei Wang Guanyu Yang agris 2022-10-09 application/pdf https://doi.org/10.3390/rs14195040 EN eng Multidisciplinary Digital Publishing Institute Atmospheric Remote Sensing https://dx.doi.org/10.3390/rs14195040 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 14; Issue 19; Pages: 5040 Arctic stratospheric ozone precipitation prediction WACCM statistical linear model Text 2022 ftmdpi https://doi.org/10.3390/rs14195040 2023-08-01T06:48:38Z An analysis of the relationship between changes in Arctic stratospheric ozone (ASO) and precipitation in eastern North America (38°–54°N, 65°–87°W; PENA) was performed using observational and reanalysis data coupled with the Whole Atmosphere Community Climate Model version 4 (WACCM4). We found that March ASO exhibits a strong correlation with PENA in April, indicating that the one-month leading ASO exerts a potentially strong impact on April PENA. Changes in tropospheric circulation over the North Pacific and North America can be influenced by ASO anomalies via stratosphere–troposphere interactions. Increased ASO typically results in the transport of drier, colder air from northwest to eastern North America and suppresses local convective activity by enhancing regional downwelling. These conditions lead to a decrease in regional atmospheric water vapor content (1000–600 hPa). Abnormally high ASO may therefore suppress precipitation, whereas abnormally low ASO serves to enhance precipitation, and the finding is supported by WACCM4 simulations incorporating these ASO anomaly signals. We also present an ASO-based statistical linear model for predicting April PENA. Results confirm that the linear model reproduces April PENA for both training and testing periods, based on March ASO, demonstrating the reliability and stability of this linear model. This study verifies that ASO is a viable predictor for projecting April PENA and thus improving forecasts of regional seasonal precipitation. Text Arctic MDPI Open Access Publishing Arctic Pacific Pena ENVELOPE(40.562,40.562,63.490,63.490) Remote Sensing 14 19 5040
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Arctic stratospheric ozone
precipitation
prediction
WACCM
statistical linear model
spellingShingle Arctic stratospheric ozone
precipitation
prediction
WACCM
statistical linear model
Xuan Ma
Fei Xie
Xiaosong Chen
Lei Wang
Guanyu Yang
Identifying a Leading Predictor of Arctic Stratospheric Ozone for April Precipitation in Eastern North America
topic_facet Arctic stratospheric ozone
precipitation
prediction
WACCM
statistical linear model
description An analysis of the relationship between changes in Arctic stratospheric ozone (ASO) and precipitation in eastern North America (38°–54°N, 65°–87°W; PENA) was performed using observational and reanalysis data coupled with the Whole Atmosphere Community Climate Model version 4 (WACCM4). We found that March ASO exhibits a strong correlation with PENA in April, indicating that the one-month leading ASO exerts a potentially strong impact on April PENA. Changes in tropospheric circulation over the North Pacific and North America can be influenced by ASO anomalies via stratosphere–troposphere interactions. Increased ASO typically results in the transport of drier, colder air from northwest to eastern North America and suppresses local convective activity by enhancing regional downwelling. These conditions lead to a decrease in regional atmospheric water vapor content (1000–600 hPa). Abnormally high ASO may therefore suppress precipitation, whereas abnormally low ASO serves to enhance precipitation, and the finding is supported by WACCM4 simulations incorporating these ASO anomaly signals. We also present an ASO-based statistical linear model for predicting April PENA. Results confirm that the linear model reproduces April PENA for both training and testing periods, based on March ASO, demonstrating the reliability and stability of this linear model. This study verifies that ASO is a viable predictor for projecting April PENA and thus improving forecasts of regional seasonal precipitation.
format Text
author Xuan Ma
Fei Xie
Xiaosong Chen
Lei Wang
Guanyu Yang
author_facet Xuan Ma
Fei Xie
Xiaosong Chen
Lei Wang
Guanyu Yang
author_sort Xuan Ma
title Identifying a Leading Predictor of Arctic Stratospheric Ozone for April Precipitation in Eastern North America
title_short Identifying a Leading Predictor of Arctic Stratospheric Ozone for April Precipitation in Eastern North America
title_full Identifying a Leading Predictor of Arctic Stratospheric Ozone for April Precipitation in Eastern North America
title_fullStr Identifying a Leading Predictor of Arctic Stratospheric Ozone for April Precipitation in Eastern North America
title_full_unstemmed Identifying a Leading Predictor of Arctic Stratospheric Ozone for April Precipitation in Eastern North America
title_sort identifying a leading predictor of arctic stratospheric ozone for april precipitation in eastern north america
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/rs14195040
op_coverage agris
long_lat ENVELOPE(40.562,40.562,63.490,63.490)
geographic Arctic
Pacific
Pena
geographic_facet Arctic
Pacific
Pena
genre Arctic
genre_facet Arctic
op_source Remote Sensing; Volume 14; Issue 19; Pages: 5040
op_relation Atmospheric Remote Sensing
https://dx.doi.org/10.3390/rs14195040
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs14195040
container_title Remote Sensing
container_volume 14
container_issue 19
container_start_page 5040
_version_ 1774714522399932416