about
Quantifying the Intra-Regional Precipitation Variability in Northwestern China over the Past 1,400 YearsENSO elicits opposing responses of semi-arid vegetation between Hemispheres.The influence of sampling design on tree-ring-based quantification of forest growth.Impacts of El Niño Southern Oscillation on the global yields of major crops.Strong influence of El Niño Southern Oscillation on flood risk around the world.Global monsoon precipitation responses to large volcanic eruptions.A Picea crassifolia Tree-Ring Width-Based Temperature Reconstruction for the Mt. Dongda Region, Northwest China, and Its Relationship to Large-Scale Climate Forcing.A 1000-Year Carbon Isotope Rainfall Proxy Record from South African Baobab Trees (Adansonia digitata L.).A Regional Stable Carbon Isotope Dendro-Climatology from the South African Summer Rainfall AreaClimate Response of Tree Radial Growth at Different Timescales in the Qinling MountainsInfluences of volcano eruptions on Asian Summer Monsoon over the last 110 years.Multi-century tree-ring precipitation record reveals increasing frequency of extreme dry events in the upper Blue Nile River catchment.Persistent drying in the tropics linked to natural forcing.Role of eruption season in reconciling model and proxy responses to tropical volcanism.Tropical explosive volcanic eruptions can trigger El Niño by cooling tropical AfricaThe paleoclimate context and future trajectory of extreme summer hydroclimate in eastern Australia.Internal ocean-atmosphere variability drives megadroughts in Western North America.Interannual to centennial variability of the South Asian summer monsoon over the past millenniumMultidecadal variations in Southern Hemisphere atmospheric 14C: Evidence against a Southern Ocean sink at the end of the Little Ice Age CO2 anomalyWas the Little Ice Age more or less El Niño-like than the Medieval Climate Anomaly? Evidence from hydrological and temperature proxy dataDrought variation of western Chinese Loess Plateau since 1568 and its linkages with droughts in western North AmericaInterdecadal hydroclimate teleconnections between Asia and North America over the past 600 yearsImpacts of a Pinatubo-size volcanic eruption on ENSOThe importance of ENSO phase during volcanic eruptions for detection and attributionDetecting changes in marine responses to ENSO from 850 to 2100 C.E.: Insights from the ocean carbon cycleLong-term stationarity of El Niño–Southern Oscillation teleconnections in southeastern AustraliaAre estimates of anthropogenic and natural influences on Australia’s extreme 2010–2012 rainfall model-dependent?Comparing proxy and model estimates of hydroclimate variability and change over the Common EraSouthern Hemisphere rainfall variability over the past 200 yearsENSO teleconnections with Australian rainfall in coupled model simulations of the last millenniumResponse of ENSO amplitude to global warming in CESM large ensemble: uncertainty due to internal variabilityThe Defining Characteristics of ENSO Extremes and the Strong 2015/2016 El NiñoFuture Changes to El Niño-Southern Oscillation Temperature and Precipitation Teleconnections
P2860
Q28647348-16AB583E-82C4-492E-B1FF-C8E208E8C14BQ30274811-7303D535-F41C-4B7F-A298-3628C327A5BAQ30799859-E258B4E6-C778-4FB1-A399-BFDDE721DDC6Q30820230-0998DCDA-BB05-4DD6-93F1-608B9F0C0BEBQ30863254-FC0F2E08-7804-4DF5-AE5E-863D03E26A53Q31072796-13E33436-43F6-4444-B758-270DE34895FDQ31120931-629F8CD8-077B-4935-BB98-A65707E5BA41Q35630445-EF8E5D91-D7B1-4245-B443-7DCA2F1E0CF7Q36079831-FFD047F0-7FE8-4A67-9C5C-9F0B2BCAEB12Q36100249-AEFFA877-9F6A-475C-BC6F-1704E5DF20C2Q37644394-202CA731-E31D-4D66-99C7-50EBC0F3AA7AQ38657006-BB2F9DF3-9E3D-4C0F-B416-3C2FF8B83EAFQ38985366-E5A27A34-A291-498E-89D2-BE3254054550Q39490582-48102141-0BDA-4A08-BB2C-B34D626DEFE7Q41924370-41A2ABAF-EE5A-469A-B4E6-E3B9D4BFB4B0Q55239849-E2311756-1143-4B77-ACF4-25B581C7065EQ55376890-9855FAE4-8272-4559-BCD4-F1308637503AQ57251463-67F5F44B-A8EB-4356-ACD8-F1CA19D77BDAQ57262838-6241E67F-A03D-4B51-BC05-DBF75C8B82BAQ57891143-AD2097C7-9E4F-4E9C-99D2-76EEB5AEA2C8Q58007247-5949D40A-4E85-4843-AB34-42D973AC3552Q58007337-DFD99B26-DF61-4A68-92D7-E1C9C56D0848Q58073040-B922E515-6497-452E-9C43-B6D402BC878EQ58074554-01F47549-E416-4BEF-847B-E9C27CBBAEB5Q58100515-F183F3E3-6290-4271-AF6C-227214C66BD2Q58238417-B710B057-3E28-4E72-A053-A863C5BEAB6FQ58238421-9FCE3D21-FB4C-4924-A78F-CF1476C21624Q58241765-784E369F-62F8-46DE-9F48-29F119F8B065Q58314920-B39CF945-2FB9-4D02-815B-737594F8779DQ58314922-D766418C-BEE2-4E52-A326-8E8F83A47E61Q58384238-A7CFF5EA-4521-4CA1-B703-4E44C51F68B7Q58393984-42081595-F44B-4B45-94A3-289350D6B964Q58412344-AFF1B754-AB50-4D50-B660-99F7C9524ED6
P2860
description
im Juli 2013 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в липні 2013
@uk
name
El Niño modulations over the past seven centuries
@en
El Niño modulations over the past seven centuries
@nl
type
label
El Niño modulations over the past seven centuries
@en
El Niño modulations over the past seven centuries
@nl
prefLabel
El Niño modulations over the past seven centuries
@en
El Niño modulations over the past seven centuries
@nl
P2093
P2860
P356
P1476
El Niño modulations over the past seven centuries
@en
P2093
Anthony M. Fowler
Duncan A. Christie
Edward R. Cook
Keyan Fang
Mariano S. Morales
Nathaniel C. Johnson
Rosanne D’Arrigo
Xiaohua Gou
P2860
P2888
P304
P356
10.1038/NCLIMATE1936
P577
2013-07-02T00:00:00Z
P5875
P6179
1024351146