Recent Progress in Sun-Earth-Climate Research: Observation and Analysis

A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Planetary Atmospheres".

Deadline for manuscript submissions: 29 April 2024 | Viewed by 1250

Special Issue Editors


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Guest Editor
Instituto de Pesquisa e Desenvolvimento (IP&D), Laboratório de Registros Naturais (Natural Records Laboratory), University of Vale do Paraíba, Av. Shishima Hifumi, 2911 - Urbanova, São José dos Campos SP 12244-390, Brazil
Interests: geomagnetism; tsunamis; ionosphere physics; physics of the sun-earth relationship (space weather); spectral analysis
Special Issues, Collections and Topics in MDPI journals

E-Mail Website
Guest Editor
Instituto de Pesquisa e Desenvolvimento (IP&D), Laboratório de Registros Naturais (Natural Records Laboratory), University of Vale do Paraíba, São José dos Campos SP 12244-390, Brazil
Interests: space weather; sun-earth interaction; study of the sun-earth-climate relationship through natural records; magnetospheric activity; interplanetary medium - space weather
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

This Special Issue aims to explore Sun–Earth–Climate relationships and natural causes using observational data and computational analysis. These climatic, solar, and natural-cause variabilities range over a time scale from the recent past (1000 years) to the present. Among the most used observational data, there are sunspots, geomagnetic, ionospheric, meteorological, climatic, and hydrological data. On the other hand, one can learn about the past of solar and climate variabilities by reading terrestrial archives that provide us with “proxy” data on the history of the Sun and climate. Bearing in mind that different natural mechanisms can affect the climate of a given place, in addition to anthropogenic effects, it is necessary to study the influence of solar activity, El Niño events, and other geophysical phenomena in order to understand climate variability. The study of solar activity, the structures of the interplanetary way, and their effects on the magnetosphere and ionosphere are also important to understand the physical dynamic processes that occur during magnetic storms, substorms, and auroras. Scientists of the Natural Records Laboratory (Laboratório de Registros Naturais - LRN) from the University of Vale do Paraíba (Universidade do Vale do Paraíba) are dedicated to expanding tree ring use and its application, as well as other observational records, to improve our understanding of past climate and environmental history,especially in Brazil and South America. Our current research focuses on the use of tree ring data networks to study regional climate, global climate teleconnections, Sun–Earth–Climate interrelationships, and anthropogenic impacts.

Dr. Virginia Klausner de Oliveira
Prof. Dr. Alan Prestes
Guest Editors

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Keywords

  • tree rings
  • climate
  • solar activity
  • Sun–Earth relationship
  • geomagnetism

Published Papers (1 paper)

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Research

17 pages, 9367 KiB  
Article
Detecting Relationship between the North–South Difference in Extreme Precipitation and Solar Cycle in China
by Jinjuan Liu, Liang Zhao, Jingsong Wang and Ziniu Xiao
Atmosphere 2024, 15(2), 175; https://0-doi-org.brum.beds.ac.uk/10.3390/atmos15020175 - 30 Jan 2024
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Abstract
The sun plays a crucial role as the primary source of energy for the Earth’s climate system and the issue of the influence of solar activity on the climate has been actively discussed recently. However, the precise impact of solar activity on extreme [...] Read more.
The sun plays a crucial role as the primary source of energy for the Earth’s climate system and the issue of the influence of solar activity on the climate has been actively discussed recently. However, the precise impact of solar activity on extreme precipitation on the decadal timescale remains insufficiently confirmed. In this study, we investigate the relationship between summer extreme precipitation events exceeding 20 mm (R20mm) in China and the 11-year sunspot number (SSN) cycle from 1951 to 2018. Results showed that the first mode of June–July R20mm, a “south-drought and north-flooding (SDNF)” distribution, exhibited a significant correlation with the SSN cycle (p = 0.02). The fundamental driver is likely the pronounced periodic response of stratospheric ozone to solar forcing. During summer of the high-solar-activity years (HSY), there is a notable increase in ozone concentration and high temperatures in the stratosphere, particularly in the Southern Hemisphere. This phenomenon leads to a layer of anomalous temperature inversion, suppressing convection at the subtropics. This induced downward anomalous airflow toward the north stimulates convective activity in the equatorial region and generates northward wave activities. These wave activities produce rising and sinking anomalies at different latitudes in the Northern Hemisphere troposphere, finally causing the “SDNF” pattern in China. Full article
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