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
wiley +1 more source
Evaluation of the Ability of CMIP6 to Simulate the Wind Speed of 10 Meters of the Arctic Region
The improvement of the ability of climate model to simulate the wind speed of 10 meters near the surface in the Arctic region plays an important role in predicting the future climate change in this region.Thirty-two CMIP6 (Coupled Model Intercomparison ...
Haoyu WU +5 more
doaj +1 more source
How Well Is Surface Diurnal Temperature Range Represented by Observations at 2‐m Level
We demonstrate that geostationary satellites depict well the Diurnal Temperature Range (DTR) in the US but differ from information at 2 m level from model outputs. Upper: mean diurnal temperature range (DTR) using GOES‐E based land surface temperature (LST) for January (left) and July (right) during 2004–2009. Lower: mean diurnal temperature range (DTR)
Rachel T. Pinker +4 more
wiley +1 more source
Compound heatwave events are heatwaves that occur simultaneously during the day and at night, which not only threaten human health but also impede sustainable socio-economic and ecosystem development.In recent years, the frequency of compound heatwave ...
Huning CHEN +3 more
doaj +1 more source
Long-term analysis of the Antarctic total ozone zonal asymmetry by MERRA-2 and CMIP6 data
Objectives. To analyze ozone monthly mean data from the MERRA-2 reanalysis and CMIP6 model. To determine Antarctic ozone asymmetry climatology for austral spring months (September, October, November) over the 1980–2014 period. Methods.
O. Ivaniha
doaj +1 more source
A higher-resolution version of the Max Planck Institute Earth System Model (MPI-ESM1.2-HR) [PDF]
The MPI‐ESM1.2 is the latest version of the Max Planck Institute Earth System Model and is the baseline for the Coupled Model Intercomparison Project Phase 6 and current seasonal and decadal climate predictions.
Baehr, J. +20 more
core +2 more sources
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
What Do Latest CMIP6 Global Climate Models Say About Future Arctic Sea Ice Coverage Changes?
Modelling of sea ice dynamics has significantly improved between CMIP5 and CMIP6, with nearly three times as many models capturing realistic annual variability in sea ice extent (SIE). What we previously thought was a non‐linear pattern of low SIE observations in 2007–2010 that would continue throughout time now appears to be non‐record‐setting lows in
Jessica L. Matthews +4 more
wiley +1 more source
The separation of the East Australian Current: A Lagrangian approach to potential vorticity and upstream control [PDF]
The East Australian Current (EAC) is the western boundary current flowing along the east coast of Australia separating from the coast at approximately 34°S.
Kiss, AE +3 more
core +1 more source
Solar Geoengineering Effects on Malaria Transmission Risk in South Asia Under G6sulfur Scenario
Comparison of EIR (unit: No of infected bites per person per day) for each considered country in South Asia, under the considered scenarios, averaged over the period 2020–2090. A regression equation is shown for each country (for Bhutan EIRG = 0.1690 × 10−10 EIRS + 0.5968 × 10−12) to illustrate the projected trend.
Athar Hussain +2 more
wiley +1 more source

