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Sunshine Duration in Brazil From Meteosat (1983–2020): Climatology, Variability and Long‐Term Trends
Using nearly four decades of Meteosat satellite data (1983–2020), this study presents a country‐wide climatology of sunshine duration (SDU) in Brazil. The results reveal marked regional contrasts, dominant modes of variability, and significant long‐term trends, providing new information on the most relevant meteorological systems that influence SDU and
Maria Lívia Lins Mattos Gava +2 more
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Projected Annual and Monsoonal Precipitation Trends of CMIP6 Over Peninsular Malaysia
In this study, we examined historical and projected precipitation temporal trends across Peninsular Malaysia using ground‐based records and CMIP6 models from NEX‐GDDP. Analysing data from 518 reliable gauges over 1973–2022, it identified spatial and monsoonal variations.
Nurul Afiqah Mohamad Arbai +1 more
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The graphical abstract presents observed (1963–2023) and projected changes in hydroclimatic extremes in Rio Grande do Norte, Brazil. It integrates dry‐spell duration (CDD) and extreme precipitation (R95pTOT) using CMIP6 multimodel ensembles under SSP1‐2.6, SSP2‐4.5, and SSP5‐8.5.
Daris Correia dos Santos
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Performance Evaluation of the MPAS Model in Simulating Southeast Asian Rainfall Characteristics
This study evaluates the performance of the Model for Prediction Across Scales–Atmosphere (MPAS) in reproducing key rainfall characteristics over Southeast Asia (SEA) during 2000–2020, using the MSWEP dataset as reference. MPAS realistically captures the observed meridional rainfall gradient, with higher rainfall in the south and lower in the north, as
Nguyen Thanh Hung +4 more
wiley +1 more source
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1992
The coastal zone lies between terrestrial and marine systems. It includes the entirety of the coastal plains, the continental shelves and their waters, and bays, estuaries, lagoons, dune fields, and deltas (Inman and Nordstrom 1971; Ketchum 1972; Inman and Brush 1973; Fig. 21.1).
G. Carleton Ray, Bruce P. Hayden
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The coastal zone lies between terrestrial and marine systems. It includes the entirety of the coastal plains, the continental shelves and their waters, and bays, estuaries, lagoons, dune fields, and deltas (Inman and Nordstrom 1971; Ketchum 1972; Inman and Brush 1973; Fig. 21.1).
G. Carleton Ray, Bruce P. Hayden
openaire +1 more source

