npj Climate and Atmospheric Science

(The median citation count of npj Climate and Atmospheric Science is 3. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 500 papers]. The publications cover those that have been published in the past four years, i.e., from 2019-08-01 to 2023-08-01.)
Biomass waste utilisation in low-carbon products: harnessing a major potential resource209
Half the world’s population are exposed to increasing air pollution141
Improved calculation of warming-equivalent emissions for short-lived climate pollutants133
Designing vegetation barriers for urban air pollution abatement: a practical review for appropriate plant species selection114
‘Eastern African Paradox’ rainfall decline due to shorter not less intense Long Rains63
Increased European heat waves in recent decades in response to shrinking Arctic sea ice and Eurasian snow cover60
Lifecycle of light-absorbing carbonaceous aerosols in the atmosphere59
Causes of large projected increases in hurricane precipitation rates with global warming55
Australia’s Black Summer pyrocumulonimbus super outbreak reveals potential for increasingly extreme stratospheric smoke events55
Anthropogenic warming and intraseasonal summer monsoon variability amplify the risk of future flash droughts in India53
Decadal predictability of North Atlantic blocking and the NAO50
Warming and drying over the central Himalaya caused by an amplification of local mountain circulation49
The Cape Town “Day Zero” drought and Hadley cell expansion47
Frequency of severe thunderstorms across Europe expected to increase in the 21st century due to rising instability47
Increased rainfall stimulates permafrost thaw across a variety of Interior Alaskan boreal ecosystems47
Future exacerbation of hot and dry summer monsoon extremes in India46
Increased occurrence of high impact compound events under climate change46
Business-as-usual will lead to super and ultra-extreme heatwaves in the Middle East and North Africa43
Nowcasting lightning occurrence from commonly available meteorological parameters using machine learning techniques42
Exploring dependence of COVID-19 on environmental factors and spread prediction in India41
Future changes in monsoon duration and precipitation using CMIP640
Incorrect Asian aerosols affecting the attribution and projection of regional climate change in CMIP6 models39
On the curious case of the recent decade, mid-spring precipitation deficit in central Europe39
Estimating global mean sea-level rise and its uncertainties by 2100 and 2300 from an expert survey38
Sea ice and atmospheric circulation shape the high-latitude lapse rate feedback36
Historical total ozone radiative forcing derived from CMIP6 simulations35
Ocean fertilization by pyrogenic aerosol iron34
Global climatology and trends in convective environments from ERA5 and rawinsonde data33
Further improvement of warming-equivalent emissions calculation32
Serial clustering of extratropical cyclones: a review of where, when and why it occurs32
Intraseasonal variability of global land monsoon precipitation and its recent trend30
Using UNSEEN trends to detect decadal changes in 100-year precipitation extremes30
Trends in United States large hail environments and observations29
Sea-spray regulates sulfate cloud droplet activation over oceans28
Indicate separate contributions of long-lived and short-lived greenhouse gases in emission targets28
Better monsoon precipitation in coupled climate models due to bias compensation26
Amplified risk of spatially compounding droughts during co-occurrences of modes of natural ocean variability26
Urban warming and future air-conditioning use in an Asian megacity: importance of positive feedback25
Stochastic nucleation processes and substrate abundance explain time-dependent freezing in supercooled droplets25
Increasing heat and rainfall extremes now far outside the historical climate24
Changes in temporal inequality of precipitation extremes over China due to anthropogenic forcings24
Non-CO2 forcing changes will likely decrease the remaining carbon budget for 1.5 °C24
Advanced risk-based event attribution for heavy regional rainfall events24
The impacts of the atmospheric boundary layer on regional haze in North China24
Seasonal to multi-year soil moisture drought forecasting23
Robust observations of land-to-atmosphere feedbacks using the information flows of FLUXNET23
Northern Hemisphere drought risk in a warming climate22
Formation of secondary organic aerosols from anthropogenic precursors in laboratory studies22
The growing importance of oceanic moisture sources for continental precipitation22
Tropical storms trigger phytoplankton blooms in the deserts of north Indian Ocean21
Predicting global patterns of long-term climate change from short-term simulations using machine learning21
A 3D study on the amplification of regional haze and particle growth by local emissions20
Significant ground-level ozone attributed to lightning-induced nitrogen oxides during summertime over the Mountain West States20
Linking midlatitudes eddy heat flux trends and polar amplification19
Role of synoptic activity on projected changes in upwelling-favourable winds at the ocean’s eastern boundaries18
Impacts of Atlantic multidecadal variability on the tropical Pacific: a multi-model study18
Atlantic Ocean influence on Middle East summer surface air temperature18
Co-benefits of reducing PM2.5 and improving visibility by COVID-19 lockdown in Wuhan18
Large-scale controls of propagation of the Madden-Julian Oscillation18
Global increase in wildfire potential from compound fire weather and drought17
Drivers behind the summer 2010 wave train leading to Russian heatwave and Pakistan flooding17
Connecting the dots: NOx emissions along a West Siberian natural gas pipeline17
Author Correction: Estimating global mean sea-level rise and its uncertainties by 2100 and 2300 from an expert survey17
Neglecting irrigation contributes to the simulated summertime warm-and-dry bias in the central United States17
Seasonality and reduced nitric oxide titration dominated ozone increase during COVID-19 lockdown in eastern China17
Sharp rises in large-scale, long-duration precipitation extremes with higher temperatures over Japan16
Likelihood of unprecedented drought and fire weather during Australia’s 2019 megafires16
NAO predictability from external forcing in the late 20th century16
Mt. Everest’s highest glacier is a sentinel for accelerating ice loss15
Formation and composition of the UTLS aerosol15
Addressing nitrogenous gases from croplands toward low-emission agriculture15
Dynamics and characteristics of dry and moist heatwaves over East Asia15
Global phosphorus dynamics in terms of phosphine14
Amplification of synoptic to annual variability of West African summer monsoon rainfall under global warming14
Seasonal climate forecast can inform the European agricultural sector well in advance of harvesting14
A multiscale model for El Niño complexity14
Dark air–liquid interfacial chemistry of glyoxal and hydrogen peroxide13
A possible relation between Arctic sea ice and late season Indian Summer Monsoon Rainfall extremes13
Constraining Amazonian land surface temperature sensitivity to precipitation and the probability of forest dieback13
Soil moisture signature in global weather balloon soundings13
Recent frontiers of climate changes in East Asia at global warming of 1.5°C and 2°C12
Record low sea ice extent in the Weddell Sea, Antarctica in April/May 2019 driven by intense and explosive polar cyclones12
Diurnal self-aggregation12
On the future zonal contrasts of equatorial Pacific climate: Perspectives from Observations, Simulations, and Theories11
Contrasting response of hydrological cycle over land and ocean to a changing CO2 pathway11
Variations in sub-daily precipitation at centennial scale11
Implications for ozone control by understanding the survivor bias in observed ozone-volatile organic compounds system11
Ecological and societal effects of Central Asian streamflow variation over the past eight centuries11
Beyond megacities: tracking air pollution from urban areas and biomass burning in Brazil11
Human-caused long-term changes in global aridity11
Low-dimensional representations of Niño 3.4 evolution and the spring persistence barrier10
Intensity changes of Indian Ocean dipole mode in a carbon dioxide removal scenario10
Constraint on precipitation response to climate change by combination of atmospheric energy and water budgets10
Coupled stratosphere-troposphere-Atlantic multidecadal oscillation and its importance for near-future climate projection10
Improvements and persistent biases in the southeast tropical Atlantic in CMIP models10
Formation of decimeter-scale, long-lived elevated ionic conductivity regions in thunderclouds10
Global-scale constraints on light-absorbing anthropogenic iron oxide aerosols9
Tropical rainfall subseasonal-to-seasonal predictability types9
Aerosol-induced modification of organised convection and top-of-atmosphere radiation9
A diurnal story of Δ17O($$\rm{NO}_{3}^{-}$$) in urban Nanjing and its implication for nitrate aerosol formation9
The underappreciated role of anthropogenic sources in atmospheric soluble iron flux to the Southern Ocean9
Attribution of late summer early autumn Arctic sea ice decline in recent decades9
The role of future anthropogenic methane emissions in air quality and climate9
Changes in Hadley circulation and intertropical convergence zone under strategic stratospheric aerosol geoengineering9
Early-onset of Atlantic Meridional Overturning Circulation weakening in response to atmospheric CO2 concentration9
Missing eddy feedback may explain weak signal-to-noise ratios in climate predictions8
Long-lead ENSO control of the boreal summer intraseasonal oscillation in the East Asian-western North Pacific region8
Single- and multi-year ENSO events controlled by pantropical climate interactions8
Quantifying the role of ocean coupling in Arctic amplification and sea-ice loss over the 21st century8
Source forensics of inorganic and organic nitrogen using δ15N for tropospheric aerosols over Mt. Tai8
West coast India’s rainfall is becoming more convective8
Sea ice loss of the Barents-Kara Sea enhances the winter warming over the Tibetan Plateau8
Seasonal-to-decadal prediction of El Niño–Southern Oscillation and Pacific Decadal Oscillation7
Atmospheric feedback explains disparate climate response to regional Arctic sea-ice loss7
Large hemispheric differences in the Hadley cell strength variability due to ocean coupling7
Anthropogenic warming disrupts intraseasonal monsoon stages and brings dry-get-wetter climate in future East Asia7
Arctic amplification, and its seasonal migration, over a wide range of abrupt CO2 forcing7
Analysis of factors influencing tropical lower stratospheric water vapor during 1980–20177
Bioaerosols and dust are the dominant sources of organic P in atmospheric particles7
ESA-ECMWF Report on recent progress and research directions in machine learning for Earth System observation and prediction7
New particle formation from agricultural recycling of organic waste products7
Low Antarctic continental climate sensitivity due to high ice sheet orography7
Heatwave–blocking relation change likely dominates over decrease in blocking frequency under global warming6
Arabian Sea Aerosol-Indian Summer Monsoon Rainfall relationship and its modulation by El-Nino Southern Oscillation6
Investigating the impact of cloud-radiative feedbacks on tropical precipitation extremes6
Size-dependent aerosol iron solubility in an urban atmosphere6
Relationship between Azores High and Indian summer monsoon6
Resolution dependence of CO2-induced Tropical Atlantic sector climate changes6
The fast response of Sahel precipitation to climate change allows effective mitigation action6
Estimation of hygroscopic growth properties of source-related sub-micrometre particle types in a mixed urban aerosol6
Impact of vertical air motions on ice formation rate in mixed-phase cloud layers6
Seasonal predictability of baroclinic wave activity6
Machine learning prediction of the Madden-Julian oscillation6
The effect of rapid adjustments to halocarbons and N2O on radiative forcing6
Feedbacks and eddy diffusivity in an energy balance model of tropical rainfall shifts5
Four distinct Northeast US heat wave circulation patterns and associated mechanisms, trends, and electric usage5
Arctic Oscillation and Pacific-North American pattern dominated-modulation of fire danger and wildfire occurrence5
Increased aerosol concentrations in the High Arctic attributable to changing atmospheric transport patterns5
West African monsoon precipitation impacted by the South Eastern Atlantic biomass burning aerosol outflow5
Urban climate changes during the COVID-19 pandemic: integration of urban-building-energy model with social big data5
Predictability of South-Asian monsoon rainfall beyond the legacy of Tropical Ocean Global Atmosphere program (TOGA)5
Aerosol-boundary layer interaction modulated entrainment process5
Linkage between precipitation isotopes and biosphere-atmosphere interaction observed in northeast India5
Neutral modes of surface temperature and the optimal ocean thermal forcing for global cooling5
Historical predictability of rainfall erosivity: a reconstruction for monitoring extremes over Northern Italy (1500–2019)5
Quantifying non-CO2 contributions to remaining carbon budgets5
A global perspective on western Mediterranean precipitation extremes5
Global-scale interdecadal variability a skillful predictor at decadal-to-multidecadal timescales for Sahelian and Indian Monsoon Rainfall5
Disentangling drivers of air pollutant and health risk changes during the COVID-19 lockdown in China5
Two different propagation patterns of spatiotemporally contiguous heatwaves in China5
Moisture channels and pre-existing weather systems for East Asian rain belts5
Increasing atmospheric dust transport towards the western Mediterranean over 1948–20205
Three-dimensional structure and transport pathways of dust aerosols over West Asia5
The critical role of dimethylamine in the rapid formation of iodic acid particles in marine areas5
Author Correction: Increased rainfall stimulates permafrost thaw across a variety of Interior Alaskan boreal ecosystems4
Dominant controls of cold-season precipitation variability over the high mountains of Asia4
Multi-annual prediction of drought and heat stress to support decision making in the wheat sector4
Dynamical and moist thermodynamical processes associated with Western Ghats rainfall decadal variability4
Meteorological flash droughts risk projections based on CMIP6 climate change scenarios4
A sea-level monopole in the equatorial Indian Ocean4
Trends in spectrally resolved outgoing longwave radiation from 10 years of satellite measurements4
Comparing deuterium excess to large-scale precipitation recycling models in the tropics3
Indian Ocean Dipole and ENSO’s mechanistic importance in modulating the ensuing-summer precipitation over Eastern China3
Forest canopy mitigates soil N2O emission during hot moments3
The role of the Pacific Decadal Oscillation and ocean-atmosphere interactions in driving US temperature predictability3
Local meridional circulation changes contribute to a projected slowdown of the Indian Ocean Walker circulation3
Seasonal variation of dry and wet islands in Beijing considering urban artificial water dissipation3
A method to dynamically constrain black carbon aerosol sources with online monitored potassium3
Changes in land-atmosphere coupling increase compound drought and heatwaves over northern East Asia3
ENSO influence on Bay of Bengal cyclogenesis confined to low latitudes3
Stronger decadal variability of the Kuroshio Extension under simulated future climate change3
VARENN: graphical representation of periodic data and application to climate studies3
Increasing activity of tropical cyclones in East Asia during the mature boreal autumn linked to long-term climate variability3
Monitoring global climate change using GNSS radio occultation3
Asian-Australian summer monsoons linkage to ENSO strengthened by global warming3
An analytic model of the tropical cyclone outer size3
Indian Ocean warming as key driver of long-term positive trend of Arctic Oscillation3
Weak Hadley cell intensity changes due to compensating effects of tropical and extratropical radiative forcing3