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Serafino Afonso Rui Mucova, Ulisses Miranda Azeiteiro, Walter Leal Filho, Carina Lurdes Lopes, João Miguel Dias and Mário Jorge Pereira
Mean sea-level is expected to rise significantly by 2100 in all scenarios, including those compatible with the objectives of the Paris Climate Agreement. Global sea level rise projections indicate devastating implications for populations, ecosystem servi...
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Anubhav Goyal,Joana Pereira
Pág. 79 - 98
Increase in water induced risks are realized with marginal settlements being more vulnerable due to limited adaptive capacity. The challenge put forward by climate change, in absence of adequate formal strategies, has forced the dwellers of marginal sett...
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Lucrêncio Silvestre Macarringue, Édson Luis Bolfe, Soltan Galano Duverger, Edson Eyji Sano, Marcellus Marques Caldas, Marcos César Ferreira, Jurandir Zullo Junior and Lindon Fonseca Matias
Accurate land use and land cover (LULC) mapping is essential for scientific and decision-making purposes. The objective of this paper was to map LULC classes in the northern region of Mozambique between 2011 and 2020 based on Landsat time series processe...
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Linfei Bai, Haibin Lü, Haojie Huang, Shahzad Muhammad Imran, Xiaoqi Ding and Yuanzhi Zhang
The unique tropical storm (TS) Deliwe (2014) occurred in the northern Mozambique Channel on 17 January 2014 and turned right during its whole life cycle, moving south along the west coast of Madagascar Island. During the development of the TS, the anticy...
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Limbikani C. Banda, Michael O. Rivett, Robert M. Kalin, Anold S. K. Zavison, Peaches Phiri, Geoffrey Chavula, Charles Kapachika, Sydney Kamtukule, Christina Fraser and Muthi Nhlema
Integrated Water Resources Management (IWRM) is vital to the future of Malawi and motivates this study?s provision of the first stable isotope baseline characterization of the Shire River Basin (SRB). The SRB drains much of Southern Malawi and receives t...
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Peter R. Johnson, Galen P. Halverson, Timothy M. Kusky, Robert J. Stern and Victoria Pease
The Arabian-Nubian Shield (ANS) includes Middle Cryogenian-Ediacaran (790?560 Ma) sedimentary and volcanic terrestrial and shallow-marine successions unconformable on juvenile Cryogenian crust. The oldest were deposited after 780?760 Ma shearing and sutu...
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