Results 201 to 210 of about 57,002 (295)

Diagnosis of the Contribution of Internal Climate Variability to Global Surface Temperature Projection Under Future Warming

Geophysical Research Letters, Volume 53, Issue 10, 28 May 2026.
Abstract Internal climate variability (ICV) is a critical source of uncertainty in global surface temperature (GST) projections. We find regional drivers of ICV in GST projections and investigate their evolution under anthropogenic forcing. Among four CMIP6 large ensemble simulations under historical and SSP5‐8.5 scenarios, we focus on MIROC6 and ...
Sae‐Yoon Oh, Sang‐Wook Yeh, Benjamin P. Kirtman   +2 more
wiley   +1 more source

Atmospheric stability sets maximum moist heat and convection in the midlatitudes. [PDF]

Sci Adv
Li F, Tamarin-Brodsky T.
europepmc   +1 more source

Climate Change Amplifies Rainfall Sensitivity to Deforestation in the Southern Amazon

Geophysical Research Letters, Volume 53, Issue 9, 16 May 2026.
Abstract Rainfall among the Amazon has been shown to decline sharply once forest loss exceeds a critical threshold, typically around 30%–40%. However, future interactions between climate change and deforestation on this threshold remain unclear. We model their combined effects by 2050 on rainfall and temperature.
Jie Zhang, Alice Catherine Hughes, Britaldo Silveira Soares‐Filho, Jose Antonio Marengo, Eduardo Eiji Maeda   +4 more
wiley   +1 more source

Trends in vertical wind velocity variability reveal cloud microphysical feedback. [PDF]

Nat Commun
Barahona D, Breen KH, Ngo D, Maciel FV, Patnaude R, Diao M.   +5 more
europepmc   +1 more source

Simulating Shallow Mesoscale Overturning Circulations in the Trades With Kilometer‐Scale Earth System Models

Geophysical Research Letters, Volume 53, Issue 9, 16 May 2026.
Abstract Shallow mesoscale overturning circulations (SMOCs) are ubiquitous in the trades, primarily triggered by mesoscale convective heating and influencing the organization of shallow cumuli. Accurate representation of SMOCs and their co‐variability with moisture is crucial for capturing mesoscale cloud organization in models and improving climate ...
Ian C. D. V. Dragaud, Raphaela Vogel, Juan Pedro Mellado, Tobias Becker   +3 more
wiley   +1 more source

Rapid Indian Ocean warming fuels more frequent extreme pre-flood season rainfall over southern China. [PDF]

Natl Sci Rev
Hou R, Zhang W, Hu S, Xu R.
europepmc   +1 more source

Attributing Upper‐Tropospheric Warm Biases in CMIP6 Models to Ice Cloud‐Radiation Interaction Deficiencies Over Tropical Oceans

Geophysical Research Letters, Volume 53, Issue 9, 16 May 2026.
Abstract We assess the impact of hydrometeor radiative effects on tropical and subtropical Pacific air temperature anomalies (TAA) using Coupled Model Intercomparison Project Phase 6 (CMIP6) model simulations and satellite data. CMIP6 models are grouped by their treatment of frozen hydrometeors: SON2 (explicit cloud and falling ice), SON1 (simplified),
J.‐L. F. Li, Wei‐Liang Lee, Kuan‐Man Xu, J. H. Jiang, Yi‐Hui Wang, Yu‐Cian Tsai, S‐P. Ho, Qing Yue, Graeme Stephens, Jia‐Yuh Yu, Huiwen Chuang   +10 more
wiley   +1 more source

Role of Future Climate Change, Air Pollution Control and Methane Mitigation in Driving Hydroxyl Radical (OH) and Methane Lifetime

Geophysical Research Letters, Volume 53, Issue 9, 16 May 2026.
Abstract The hydroxyl radical (OH) determines the atmospheric lifetime of many pollutants like methane (CH4 ${\text{CH}}_{4}$). This study isolates climate change, air pollution control and CH4 ${\text{CH}}_{4}$ mitigation effects on OH concentrations ([OH]) and CH4 ${\text{CH}}_{4}$ lifetime, by analyzing Coupled Model Intercomparison Project Phase 6 (
G. Chua, V. Naik, L. W. Horowitz
wiley   +1 more source

Mesoscale Convective Systems in Northeastern North America: identification and evaluation with the convection-permitting version of the Canadian Regional Climate Model. [PDF]

Clim Dyn
Alpizar M, Di Luca A, Gachon P, Roberge F.   +3 more
europepmc   +1 more source

Changes in the Westward Transport of Saharan Dust From West Africa With Anthropogenic Forcing in the WRF Model

Geophysical Research Letters, Volume 53, Issue 9, 16 May 2026.
Abstract Large uncertainties exist for future westward Saharan dust transport with increasing Greenhouse Gas emissions. We evaluate future changes in westward dust transport at the longitude of 18.6°W and a latitude range of 4°N–30°N using the Weather Research and Forecasting Model (WRF) with the GOCART dust module for the present‐day, with ERA‐Interim
Gregory S. Jenkins, Delián Colón‐Burgos, Jacob Tindan   +2 more
wiley   +1 more source