Volcanic eruptions are natural disasters that can have severe impacts on human life both locally and globally. Remote sensing using satellites enables the monitoring and tracking of volcanic clouds, even in locations with difficult or no access, and helps determine eruption source parameters (e.g., erupted volume, plume height, and mass eruption rate), which are essential for describing eruption dynamics and evaluating the associated natural risks.

A systematic literature review was conducted to understand how satellite remote sensing can be used to monitor and detect ash and SO₂. This review ranges from optical (multispectral, hyperspectral and LiDAR) to radar and thermal sensors. This review aims to identify the accuracy, advantages, and limitations of different sensors and algorithms. The Preferred Reporting Items for Systematic Reviews and Meta-analyses (PRISMA) was used to conduct the review, and the search parameters included keywords related to the review topic and articles published in peer-reviewed journals between January 1^st, 2010, to September 30^th, 2022.

From this search, 53 papers were chosen based on the use of satellites to detect and monitor volcanic clouds and estimate eruptive source parameters. This review revealed that SEVIRI, AHI, AVHRR, and MODIS are commonly used sensors because of their availability and near real-time capabilities. MISR and CALIOP are also frequently used because of their high spatial and vertical resolutions. The traditional brightness temperature difference (BTD) with radiative transfer models (RTM) is the most used approach to detect and retrieve volcanic clouds parameters despite its limitations. Hyperspectral sensors, such as IASI and TROPOMI, are commonly utilized for SO₂ detection and estimation. Limitations related to scattering, which occur during cloudy conditions, make accurate measurements difficult or impossible under extreme cloudy conditions. When used with the COBRA algorithm, the TROPOMI sensor shows improved resolution and accuracy, reducing noise and scattering.

Although individual approaches and their integration have contributed to the study of volcanic ash and SO₂ emissions, there are limitations both to remote sensing sensors and algorithms used. To overcome the limitations of current sensors and retrieval methods, future research should prioritize the integration of multi-sensor data, address limitations in spatial and temporal resolutions, and utilize computational methods, such as statistical methods, neural networks, and deep learning algorithms, to eliminate the need for fixed threshold constraints present in traditional methods.