| Atmospheric transport and deposition of microplastics in a remote mountain catchment |
138 |
| Anthropogenic stresses on the world's big rivers |
92 |
| Microplastic contamination of river beds significantly reduced by catchment-wide flooding |
90 |
| Environmental and social footprints of international trade |
82 |
| Stabilization of atmospheric nitrogen deposition in China over the past decade |
58 |
| A consensus estimate for the ice thickness distribution of all glaciers on Earth |
56 |
| Influence of diatom diversity on the ocean biological carbon pump |
55 |
| Geological and climatic influences on mountain biodiversity |
55 |
| Drought impacts on terrestrial primary production underestimated by satellite monitoring |
52 |
| A two-pollutant strategy for improving ozone and particulate air quality in China |
51 |
| Structural decline in China's CO2 emissions through transitions in industry and energy systems |
49 |
| The biomass and biodiversity of the continental subsurface |
48 |
| Consistency and discrepancy in the atmospheric response to Arctic sea-ice loss across climate models |
46 |
| Shape of (101955) Bennu indicative of a rubble pile with internal stiffness |
45 |
| Soil carbon storage informed by particulate and mineral-associated organic matter |
43 |
| Worldwide alteration of lake mixing regimes in response to climate change |
42 |
| Drivers and mechanisms of ocean deoxygenation |
41 |
| Mangrove canopy height globally related to precipitation, temperature and cyclone frequency |
39 |
| Twenty-first century glacier slowdown driven by mass loss in High Mountain Asia |
39 |
| Dryland photoautotrophic soil surface communities endangered by global change |
39 |
| Craters, boulders and regolith of (101955) Bennu indicative of an old and dynamic surface |
38 |
| Two decades of glacier mass loss along the Andes |
37 |
| Higher frequency of Central Pacific El Nino events in recent decades relative to past centuries |
37 |
| Evidence of supershear during the 2018 magnitude 7.5 Palu earthquake from space geodesy |
37 |
| Consistent multidecadal variability in global temperature reconstructions and simulations over the Common Era |
36 |
| Microbial formation of stable soil carbon is more efficient from belowground than aboveground input |
36 |
| West Antarctic Ice Sheet retreat in the Amundsen Sea driven by decadal oceanic variability |
36 |
| Recent global decline in endorheic basin water storages |
35 |
| Rapid incision of the Mekong River in the middle Miocene linked to monsoonal precipitation |
34 |
| Recent Southern Ocean warming and freshening driven by greenhouse gas emissions and ozone depletion |
33 |
| Palaeoclimate constraints on the impact of 2 degrees C anthropogenic warming and beyond |
32 |
| Rapid transition from continental breakup to igneous oceanic crust in the South China Sea |
32 |
| Global niche of marine anaerobic metabolisms expanded by particle microenvironments |
32 |
| Human domination of the global water cycle absent from depictions and perceptions |
31 |
| Early and persistent supershear rupture of the 2018 magnitude 7.5 Palu earthquake |
31 |
| Direct observation of permafrost degradation and rapid soil carbon loss in tundra |
31 |
| Amazon forest response to CO2 fertilization dependent on plant phosphorus acquisition |
30 |
| Global diffusive fluxes of methane in marine sediments |
30 |
| A vegetation control on seasonal variations in global atmospheric mercury concentrations |
29 |
| Forced subduction initiation recorded in the sole and crust of the Semail Ophiolite of Oman |
29 |
| Burma Terrane part of the Trans-Tethyan arc during collision with India according to palaeomagnetic data |
28 |
| West Antarctic ice loss influenced by internal climate variability and anthropogenic forcing |
28 |
| The geological and climatological case for a warmer and wetter early Mars |
28 |
| Massive collapse of two glaciers in western Tibet in 2016 after surge-like instability |
27 |
| Rapid expansion of northern peatlands and doubled estimate of carbon storage |
26 |
| Global lake evaporation accelerated by changes in surface energy allocation in a warmer climate |
26 |
| Southward shift of the global wind energy resource under high carbon dioxide emissions |
25 |
| Contribution of wetlands to nitrate removal at the watershed scale |
25 |
| Persistence of dissolved organic matter explained by molecular changes during its passage through soil |
24 |
| Arctic sea-ice variability is primarily driven by atmospheric temperature fluctuations |
24 |
