about
The indirect global warming potential and global temperature change potential due to methane oxidationPersistence of climate changes due to a range of greenhouse gasesIrreversible climate change due to carbon dioxide emissionsEuropean land CO2 sink influenced by NAO and East-Atlantic Pattern couplingSpring temperature change and its implication in the change of vegetation growth in North America from 1982 to 2006Contributions of past and present human generations to committed warming caused by carbon dioxide.Sensitivity of tropical carbon to climate change constrained by carbon dioxide variability.Evaluation of terrestrial carbon cycle models for their response to climate variability and to CO2 trends.Delayed detection of climate mitigation benefits due to climate inertia and variabilityA two-fold increase of carbon cycle sensitivity to tropical temperature variations.Evidence for a weakening relationship between interannual temperature variability and northern vegetation activity.Carbon cycle feedbacks and future climate change.The terrestrial biosphere as a net source of greenhouse gases to the atmosphere.Changes in climate and land use have a larger direct impact than rising CO2 on global river runoff trends.Projected land photosynthesis constrained by changes in the seasonal cycle of atmospheric CO2.Reducing uncertainties in decadal variability of the global carbon budget with multiple datasets.Environment. Tropical forests and climate policy.The impacts of climate change on water resources and agriculture in China.Permafrost carbon-climate feedbacks accelerate global warming.Late Holocene methane rise caused by orbitally controlled increase in tropical sources.Carbon cycle. The dominant role of semi-arid ecosystems in the trend and variability of the land CO₂ sink.Europe-wide reduction in primary productivity caused by the heat and drought in 2003.Comparing concentration-based (AOT40) and stomatal uptake (PODY) metrics for ozone risk assessment to European forests.Compensatory water effects link yearly global land CO2 sink changes to temperature.A unifying conceptual model for the environmental responses of isoprene emissions from plants.Forest annual carbon cost: a global-scale analysis of autotrophic respiration.Surface urban heat island across 419 global big cities.Net carbon dioxide losses of northern ecosystems in response to autumn warming.Climatic control of the high-latitude vegetation greening trend and Pinatubo effect.On the causes of trends in the seasonal amplitude of atmospheric CO2.The decreasing range between dry- and wet- season precipitation over land and its effect on vegetation primary productivity.A steep road to climate stabilization.Land use change and El Niño-Southern Oscillation drive decadal carbon balance shifts in Southeast Asia.Changes in climate extremes, fresh water availability and vulnerability to food insecurity projected at 1.5°C and 2°C global warming with a higher-resolution global climate model.Trends in the sources and sinks of carbon dioxideThe utility of the historical record for assessing the transient climate response to cumulative emissions.Greening of the Earth and its driversBiophysical and economic limits to negative CO2 emissionsThe status and challenge of global fire modellingThe Scenario Model Intercomparison Project (ScenarioMIP) for CMIP6
P50
Q21994574-459D63BF-9834-449C-B404-4663B52D6E16Q24289265-87402CD0-9668-4651-BEFE-9CA5A510F1B2Q24643362-DBF7ACB5-225B-46E9-BE99-F47E7D190501Q28601643-78BEB4B3-6057-4F0B-9A8E-C594904D2394Q28743215-40A76479-6D98-49B4-B43F-BBD0A086B55CQ28769541-08E9DBAE-FDF8-4F92-82C7-7CA0CCBC221DQ30587256-55A27276-46FE-4A78-A2FA-ACC4AA6FD8DEQ30601601-E83D0015-0F02-4978-B959-84FC75C83128Q30671774-259CCB78-2E8B-4CD1-A7C8-1166AA0C4E8FQ30742098-5EE1D502-70C6-4529-90C0-37BBB4259154Q30860434-9AAC998D-2B96-4076-BC5A-7D982EB266B4Q31001628-A8B6405D-CBFA-4FE4-9A07-2507F87BFA13Q31056278-F6D00D7F-8409-40DA-9CA7-1E9FC3A3B75EQ31129902-522CA07F-30F3-4859-BAAF-DCC6FD4E94F2Q31133572-4A756A90-FDB8-486F-8CA4-A9E801A05B94Q31140267-8B88558E-53B3-4E0F-9915-8562CC8D33EEQ33284346-0C8C6C34-0792-4441-B518-C6115E5B7963Q33681957-A80D5BD2-C1C0-4818-84B1-2E0C18617C21Q33996540-FBD5C5AB-A381-42A8-994E-59167B93F249Q34162549-892AA47C-BC22-4B90-8637-DA48353982AFQ35638909-210DE4D4-6DD2-4DEB-839D-04952C22B5FBQ38947312-C25D6AEF-71B4-4BB3-824C-D66A51C151B5Q38950843-1116B0B6-47DF-4071-AC09-DCF8A57EA5F4Q39018026-3F324F7F-7B52-448C-B939-5BC377251C34Q39268440-2D39F036-E308-4BEB-9493-1EA460FFE76FQ39930563-DA34404B-1C30-4E11-9FB7-86A7F6CE6EC1Q40010461-D9A6928F-77D6-4356-9E2E-C8A1A9B8AB21Q40137504-252FA898-8D79-4038-9CF0-7F7E4098DB4BQ42040862-7DB5DD52-9C6C-4032-82CC-D5D0DC86950AQ46306444-06CCCF45-0737-40DA-BE71-8A4966DD11A2Q47214021-288C4669-84C5-4F1E-96CB-D79140759251Q47719563-BB3EA3C7-FFAD-4DB0-81E5-F15D7837FB08Q51146242-E0FB7ABD-BD96-44EC-BB51-5D60D7CA233DQ52611837-6D8E50CD-6B50-4173-B684-89C6D84896ACQ54997101-25E37213-3860-4C95-A6A2-BF58A0516DCEQ55154550-856A73C0-BF28-464B-BA03-5E0CF3A68686Q56004946-379BF001-4B3D-4A2A-A1B2-347F93D1EA90Q56017010-86F74F94-A68A-4206-B4F1-8127C275DE1BQ56330062-15CFF58D-581C-415F-9529-272DF5AD518BQ56623905-05801BE2-C229-4A89-8497-0A2E910A7AB6
P50
description
hulumtues
@sq
researcher
@en
wetenschapper
@nl
հետազոտող
@hy
name
Pierre Friedlingstein
@ast
Pierre Friedlingstein
@en
Pierre Friedlingstein
@es
Pierre Friedlingstein
@nl
Pierre Friedlingstein
@sl
type
label
Pierre Friedlingstein
@ast
Pierre Friedlingstein
@en
Pierre Friedlingstein
@es
Pierre Friedlingstein
@nl
Pierre Friedlingstein
@sl
prefLabel
Pierre Friedlingstein
@ast
Pierre Friedlingstein
@en
Pierre Friedlingstein
@es
Pierre Friedlingstein
@nl
Pierre Friedlingstein
@sl
P106
P21
P31
P496
0000-0003-3309-4739