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Enhanced spring warming of the Tibetan Plateau amplifies summer heat stress in Eastern Europe
The Tibetan Plateau (TP), often referred to as the “Roof of the World”, has experienced rapid warming in recent decades. This warming has had...
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Elevational patterns of warming effects on plant community and topsoil properties: focus on subalpine meadows ecosystem
Climate warming profoundly affects plant biodiversity, community productivity, and soil properties in alpine and subalpine grassland ecosystems....
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Assessing the impact of global warming on windstorms in the northeastern United States using the pseudo-global-warming method
Windstorms resulting from intense synoptic-scale cyclones are an important natural hazard in the current climate of the northeastern United States,...
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Warming-induced hydrothermal anomaly over the Earth’s three Poles amplifies concurrent extremes in 2022
Climate warming is causing an increase in the frequency and severity of heatwaves and extreme precipitation events, posing a threat to both...
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The seas around China in a warming climate
Anthropogenic forcings have led to multifaceted changes in the seas around China, which include the Bohai, Yellow, East China and South China Seas,...
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Kilometer-scale global warming simulations and active sensors reveal changes in tropical deep convection
Changes in tropical deep convection with global warming are a leading source of uncertainty for future climate projections. A comparison of the...
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Distinctive changes of Asian–African summer monsoon in interglacial epochs and global warming scenario
Precipitation was claimed to increase over Asian–African summer monsoon (AAM) regions during past interglacial epochs and also under future global...
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The Warming of the Tibetan Plateau in Response to Transient and Stabilized 2.0°C/1.5°C Global Warming Targets
As “the third pole”, the Tibetan Plateau (TP) is sensitive to climate forcing and has experienced rapid warming in recent decades. This study...
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An assessment of the ENSO-monsoon teleconnection in a warming climate
The El Niño-Southern Oscillation (ENSO) and the Indian summer monsoon (ISM, or monsoon) are two giants of tropical climate. Here we assess the future...
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Diurnal warming rectification in the tropical Pacific linked to sea surface temperature front
Sharp and rapid changes in the sea surface temperature (SST) associated with fronts and the diurnal cycle can drive changes in the atmospheric...
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Escalating tropical cyclone precipitation extremes and landslide hazards in South China under Global Warming
Tropical cyclones (TCs) are expected to produce more intense precipitation under global warming. However, substantial uncertainties exist in the...
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The simulation of the Indo-Pacific warm pool SST warming trend in CMIP5 and CMIP6
This paper evaluates Indo-Pacific warm pool (IPWP) sea surface temperature (SST) warming biases of Coupled Model Intercomparison Project Phase 5...
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Variability of the Pacific subtropical cells under global warming in CMIP6 models
The Pacific subtropical cells (STCs) are shallow meridional overturning circulations connecting the tropics and subtropics, and are assumed to be an...
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Local cooling and drying induced by Himalayan glaciers under global warming
Understanding the response of Himalayan glaciers to global warming is vital because of their role as a water source for the Asian subcontinent....
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Radiative Forcing and Global Warming
Fundamental to understanding climate change is understanding the energy budget between solar and infrared radiation. Radiative forcing represents the...
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Long-term climatological trends driving the recent warming along the Angolan and Namibian coasts
The coastal regions off Angola and Namibia are renowned for their highly productive marine ecosystems in the southeast Atlantic. In recent decades,...
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Integrated changes in tropical precipitation and circulation under global warming: moist static energy budget and the role of sea surface warming pattern
This study uses the outputs of 24 models from CMIP6 to investigate the underlying mechanisms that determine the spatial pattern of the changes in...
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Future changes in rainy season characteristics over East China under continuous warming
The summer rainfall amount over East China is expected to increase along with a strengthening of the East Asian summer monsoon in a warmer climate....
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Persistent warming and anomalous biogeochemical signatures observed in the Northern Tropical Pacific Ocean during 2013–2020
During 2013–2020, the northern tropical Pacific Ocean (NTPO, 5° N–20° N) experienced a persistent surface warming of over 0.5 °C. This warming was...
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Microbial abundances and carbon use under ambient temperature or experimental warming in a southern boreal peatland
Organic peat soils occupy relatively little of the global land surface area but store vast amounts of soil carbon in northern latitudes where climate...
