Climate. Varying planetary heat sink led to global-warming slowdown and acceleration.
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Metrological challenges for measurements of key climatological observables, Part 4: Atmospheric relative humidityReconciling controversies about the 'global warming hiatus'.The role of dynamically induced variability in the recent warming trend slowdown over the Northern Hemisphere.CLIMATE CHANGE. Has there been a hiatus?On the definition and identifiability of the alleged "hiatus" in global warming.Response to Comment on "Atlantic and Pacific multidecadal oscillations and Northern Hemisphere temperatures".Early onset of industrial-era warming across the oceans and continents.Mechanism of non-appearance of hiatus in Tibetan Plateau.OCEAN CIRCULATION. Observing the Atlantic Meridional Overturning Circulation yields a decade of inevitable surprises.Comparing the model-simulated global warming signal to observations using empirical estimates of unforced noise.The Effect of Natural Multidecadal Ocean Temperature Oscillations on Contiguous U.S. Regional Temperatures.Distinctive ocean interior changes during the recent warming slowdownImpacts of high-latitude volcanic eruptions on ENSO and AMOCClimatic irregular staircases: generalized acceleration of global warming.Global Warming Attenuates the Tropical Atlantic-Pacific Teleconnection.Tracking ocean heat uptake during the surface warming hiatus.Spatiotemporal Divergence of the Warming Hiatus over Land Based on Different Definitions of Mean Temperature.Possible recent warming hiatus on the northwestern Tibetan Plateau derived from ice core records.A Hiatus of the Greenhouse Effect.Mid-2000s North Atlantic shift: Heat budget and circulation changes.Prospects for a prolonged slowdown in global warming in the early 21st century.Atmospheric footprint of the recent warming slowdown.Improved estimates of ocean heat content from 1960 to 2015.GLOBAL WARMING. Recent hiatus caused by decadal shift in Indo-Pacific heating.Correspondence: Variations in ocean heat uptake during the surface warming hiatus.The Subpolar North Atlantic Ocean Heat Content Variability and its Decomposition.Decade-long deep-ocean warming detected in the subtropical South Pacific.A strong ultraviolet pulse from a newborn type Ia supernova.Change in the magnitude and mechanisms of global temperature variability with warming.Ocean submesoscales as a key component of the global heat budget.The relation between natural variations in ocean heat uptake and global mean surface temperature anomalies in CMIP5.Recent strengthening of the stratospheric Arctic vortex response to warming in the central North Pacific.Regions of significant influence on unforced global mean surface air temperature variability in climate modelsObservations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A reviewRecent global warming hiatus dominated by low-latitude temperature trends in surface and troposphere dataThe early 20th century warming: Anomalies, causes, and consequencesIdentifying the early 2000s hiatus associated with internal climate variabilityContributions of atmospheric circulation variability and data coverage bias to the warming hiatusTowards multi-resolution global climate modeling with ECHAM6-FESOM. Part II: climate variabilityPacific origin of the abrupt increase in Indian Ocean heat content during the warming hiatus
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Climate. Varying planetary heat sink led to global-warming slowdown and acceleration.
description
2014 nî lūn-bûn
@nan
2014 թուականի Օգոստոսին հրատարակուած գիտական յօդուած
@hyw
2014 թվականի օգոստոսին հրատարակված գիտական հոդված
@hy
2014年の論文
@ja
2014年論文
@yue
2014年論文
@zh-hant
2014年論文
@zh-hk
2014年論文
@zh-mo
2014年論文
@zh-tw
2014年论文
@wuu
name
Climate. Varying planetary heat sink led to global-warming slowdown and acceleration.
@ast
Climate. Varying planetary heat sink led to global-warming slowdown and acceleration.
@en
Climate. Varying planetary heat sink led to global-warming slowdown and acceleration.
@nl
type
label
Climate. Varying planetary heat sink led to global-warming slowdown and acceleration.
@ast
Climate. Varying planetary heat sink led to global-warming slowdown and acceleration.
@en
Climate. Varying planetary heat sink led to global-warming slowdown and acceleration.
@nl
prefLabel
Climate. Varying planetary heat sink led to global-warming slowdown and acceleration.
@ast
Climate. Varying planetary heat sink led to global-warming slowdown and acceleration.
@en
Climate. Varying planetary heat sink led to global-warming slowdown and acceleration.
@nl
P2860
P356
P1433
P1476
Climate. Varying planetary heat sink led to global-warming slowdown and acceleration.
@en
P2093
Xianyao Chen
P2860
P304
P356
10.1126/SCIENCE.1254937
P407
P50
P577
2014-08-01T00:00:00Z