remotesensing-logo

Journal Browser

Journal Browser

Enhanced Satellite Perspectives of Sea Surface Temperature and Air-Sea Interaction

A special issue of Remote Sensing (ISSN 2072-4292). This special issue belongs to the section "Ocean Remote Sensing".

Deadline for manuscript submissions: closed (31 March 2026) | Viewed by 6227

Editors

1. Physical Oceanography, Oceanography Department, Alexandria University, Alexandria, Egypt
2. Marine Institute, Oranmore, H91 R673 Galway, Ireland
Interests: physical oceanography; ocean modelling; operational oceanography; climate projections; sea surface temperature; climate dynamics; marine heat waves; meridional circulation; phytoplankton; upwelling system; marine strategy framework directive

E-Mail Website
Guest Editor
Oceanography Department, Faculty of Science, Alexandria University, Alexandria 21500, Egypt
Interests: physical oceanography; ocean circulation; tidal analysis; marine heatwaves; sea level changes; air-sea interaction

E-Mail Website
Guest Editor
1. GeoHydrodynamics and Environment Research (GHER), University of Liège, Liège, Belgium
2. Oceanography Department, Faculty of Science, Alexandria University, Alexandria, Egypt
Interests: physical oceanography; sea surface temperature; sea ice concentration; marine heat waves; sea level changes and tectonics; large scale teleconnection patterns; steric effect

Special Issue Information

Dear Colleagues,

Sea surface temperatures have increased significantly over the past four decades at regional and global scales. This warming affects climate and biogeochemical cycles, ocean circulation, stratification, melting of ocean-bounding glaciers and ice sheets around Greenland and Antarctica, and the exchange of momentum, heat, and gases between the ocean and atmosphere. In addition, this accelerated warming can lead to extreme events (e.g., marine heat waves, low chlorophyll-a concentrations, storm surges) that have devastating effects on the marine ecosystem (e.g., coral bleaching, eutrophication, death of benthic communities, harmful algal blooms). Sea surface temperature, surface air temperature, and sea ice concentration have been classified as essential climate variables (ECVs) by the Global Climate Observing System (GCOS) due to their climate relevance, technical feasibility, and cost-effectiveness, as they play an important role in regulating Earth's climate system and its variability. In addition, large-scale teleconnection patterns (e.g., El Niño-Southern Oscillation, North Atlantic Oscillation) can modulate large-scale climate variability.

We invite papers which use Sea Surface Temperature, Sea Ice concentration, and chlorophyll-a remote-sensing datasets and techniques to understand spatiotemporal trends and extreme events. Furthermore, the possible relation between atmospheric forcings (i.e., Heat fluxes, wind) and large-scale teleconnection patterns with these extreme events.

Dr. Hazem Nagy
Dr. Omneya Ibrahim
Dr. Bayoumy Mohamed
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 250 words) can be sent to the Editorial Office for assessment.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-anonymized peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Remote Sensing is an international peer-reviewed open access semimonthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2700 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • sea surface temperature
  • extreme events (e.g., atmospheric and oceanic heatwaves, low chlorophyll-a)
  • climate change
  • air-sea interaction
  • biogeochemical cycle
  • large-scale teleconnection pattern
  • coral bleaching
  • sea ice concentration

Benefits of Publishing in a Special Issue

  • Ease of navigation: Grouping papers by topic helps scholars navigate broad scope journals more efficiently.
  • Greater discoverability: Special Issues support the reach and impact of scientific research. Articles in Special Issues are more discoverable and cited more frequently.
  • Expansion of research network: Special Issues facilitate connections among authors, fostering scientific collaborations.
  • External promotion: Articles in Special Issues are often promoted through the journal's social media, increasing their visibility.
  • Reprint: MDPI Books provides the opportunity to republish successful Special Issues in book format, both online and in print.

Further information on MDPI's Special Issue policies can be found here.

Published Papers (3 papers)

Order results
Result details
Select all
Export citation of selected articles as:

Research

Jump to: Other

22 pages, 5503 KB  
Article
On the Concurrence of the Atmospheric and Marine Heatwaves in the Red Sea
by Mostafa Morsy, Bayoumy Mohamed, Hazem Nagy, Ahmad E. Samman, Abdallah Abdaldym and Hassan Aboelkhair
Remote Sens. 2026, 18(9), 1302; https://doi.org/10.3390/rs18091302 - 24 Apr 2026
Viewed by 745
Abstract
Atmospheric heatwaves (AHWs) and marine heatwaves (MHWs) are intensifying under climate change, yet their coupled behavior in the Red Sea remains insufficiently quantified. This study investigates the spatial and temporal characteristics of AHWs, MHWs, and their concurrent occurrence across the Red Sea from [...] Read more.
Atmospheric heatwaves (AHWs) and marine heatwaves (MHWs) are intensifying under climate change, yet their coupled behavior in the Red Sea remains insufficiently quantified. This study investigates the spatial and temporal characteristics of AHWs, MHWs, and their concurrent occurrence across the Red Sea from 1990 to 2024 using ERA5 surface air temperature (SAT) and NOAA OISST v2.1 satellite-derived sea surface temperature (SST). Remote-sensing daily satellite-derived Level-4 (L4) OISST products were used in this study to enable spatially complete and temporally consistent detection of MHWs in this narrow, semi-enclosed basin despite contamination and coastal sampling constraints. Both SAT and SST exhibit statistically significant warming trends (p < 0.05), with basin mean increases of 0.40 ± 0.07 °C/decade and 0.31 ± 0.05 °C/decade, respectively. The strongest warming was observed in the central and northern Red Sea. This warming is accompanied by significant increases in the frequency and duration of AHWs, MHWs, and their concurrent AHW-MHW events, particularly after 2010, indicating a shift toward more frequent heatwave conditions. AHWs occur more frequently than MHWs across the Red Sea, whereas MHWs exhibit long duration, particularly in the northern Red Sea, where annual durations exceed 45–50 days/year. Concurrent AHW-MHW events account for about 66% of MHWs in the Red Sea, and their characteristics show a significant increasing trend across the entire basin. These findings identify the Red Sea as a regional hotspot of increasing concurrent heatwave events and highlight the importance of satellite-based monitoring for assessing evolving climate risks in semi-enclosed basins. Full article
Show Figures

Figure 1

17 pages, 6267 KB  
Article
Temporal and Spatial Variations in the Thermal Front in the Beibu Gulf in Winter
by Ruili Sun, Xindi Song, Shuangyan He, Peiliang Li, Yanzhen Gu and Chaojie Zhou
Remote Sens. 2025, 17(3), 469; https://doi.org/10.3390/rs17030469 - 29 Jan 2025
Cited by 2 | Viewed by 1947
Abstract
Using satellite-observed data and reanalysis data, we studied the spatiotemporal variation characteristics and dynamic mechanisms of thermal fronts in the Beibu Gulf (TFIBG). TFIBG occur in December, reach their strongest point in January in the following year, and then gradually weaken until they [...] Read more.
Using satellite-observed data and reanalysis data, we studied the spatiotemporal variation characteristics and dynamic mechanisms of thermal fronts in the Beibu Gulf (TFIBG). TFIBG occur in December, reach their strongest point in January in the following year, and then gradually weaken until they completely disappear in May. Their formation is related to the bathymetry of the Beibu Gulf. In winter, the seawater in shallow-water areas (deep-water areas) cools down more (less), and Ekman currents concurrently transport warm water from the central basin of the Beibu Gulf to the west coast, which results in the formation of a thermal front at the junction of cold and warm water. The interannual variation in TFIBG intensity is related to the northeast monsoon. The strengthened (weakened) Ekman current caused by the northeast monsoon transports more (less) warm water from the central basin of the Beibu Gulf to the west coast, forming a strong (weak) thermal front at the junction of cold and warm water on an interannual scale. The upward trend of TFIBG intensity may be related to the regional heterogeneity of climate warming. This research systematically studied TFIBG, which will help improve people’s understanding of the thermal front in the South China Sea (SCS). Full article
Show Figures

Figure 1

Other

Jump to: Research

15 pages, 71007 KB  
Technical Note
Inter-Comparison of Satellite-Based Sea Ice Concentration in the Amundsen Sea, Antarctica
by Xueqi Li and Hailun He
Remote Sens. 2023, 15(24), 5695; https://doi.org/10.3390/rs15245695 - 12 Dec 2023
Cited by 2 | Viewed by 2183
Abstract
We conducted a comparison of sea ice concentration (SIC) in the Amundsen Sea using three satellite datasets: Hadley Centre’s sea ice and sea surface temperature (HadISST1), Operational Sea Surface Temperature and Ice Analysis (OSTIA), and Advanced Microwave Scanning Radiometer 2 (AMSR2). HadISST1 has [...] Read more.
We conducted a comparison of sea ice concentration (SIC) in the Amundsen Sea using three satellite datasets: Hadley Centre’s sea ice and sea surface temperature (HadISST1), Operational Sea Surface Temperature and Ice Analysis (OSTIA), and Advanced Microwave Scanning Radiometer 2 (AMSR2). HadISST1 has the longest time period, while AMSR2 has the shortest. In terms of grid resolution, HadISST1 has the coarsest resolution, while AMSR2 has the finest. The sea ice areas (SIAs) observed in HadISST1, OSTIA, and AMSR2 are similar. We studied the decadal variations in SICs by dividing the study period into four temporal segments. We investigated the differences between HadISST1 and OSTIA for each temporal segment. HadISST1 exhibited a more pronounced positive trend compared to OSTIA between 2005 and 2010. Additionally, we compared the interannual and seasonal variations in SICs between HadISST1 and OSTIA. Lastly, it should be noted that the Amundsen Sea polynya area varies across all three datasets. Full article
Show Figures

Figure 1

Back to TopTop