Match!
Gerald A. Meehl
National Center for Atmospheric Research
350Publications
93H-index
66.4kCitations
Publications 350
Newest
#1J.-F. Lamarque (NCAR: National Center for Atmospheric Research)H-Index: 7
#2Julie M. ArblasterH-Index: 49
Last.Gerald A. Meehl (NCAR: National Center for Atmospheric Research)H-Index: 93
view all 0 authors...
#1Gerald A. Meehl (NCAR: National Center for Atmospheric Research)H-Index: 93
#2Julie M. Arblaster (Monash University)H-Index: 49
Last.Cecilia M. Bitz (UW: University of Washington)H-Index: 49
view all 8 authors...
After nearly three decades of observed increasing trends of Antarctic sea ice extent, in September-October-November 2016, there was a dramatic decrease. Here we document factors that contributed to that decrease. An atmosphere-only model with a specified positive convective heating anomaly in the eastern Indian/western Pacific Ocean, representing the record positive precipitation anomalies there in September-October-November 2016, produces an anomalous atmospheric Rossby wave response with mid- ...
#1Tongwen Wu (CMA: China Meteorological Administration)H-Index: 17
#2Aixue Hu (NCAR: National Center for Atmospheric Research)H-Index: 36
Last.Gerald A. Meehl (NCAR: National Center for Atmospheric Research)H-Index: 93
view all 5 authors...
Because of natural decadal climate variability—Atlantic multi-decadal variability (AMV) and Pacific decadal variability (PDV) —the increase of global mean surface air temperature (GMSAT) has not been monotonic although atmospheric greenhouse-gas (GHG) concentrations have been increasing continuously. It has always been a challenge regarding how to separate the effects of these two factors on GMSAT. Here, we find a physically based quasi-linear relationship between transient GMSAT and well-mixed ...
#1Lei Zhang (CU: University of Colorado Boulder)H-Index: 5
#2Weiqing Han (CU: University of Colorado Boulder)H-Index: 33
Last.Toshiaki Shinoda (A&M-CC: Texas A&M University–Corpus Christi)H-Index: 3
view all 7 authors...
#1Gerald A. Meehl (NCAR: National Center for Atmospheric Research)H-Index: 93
#2Dongxia Yang (Monash University)H-Index: 1
Last.Justin Small (NCAR: National Center for Atmospheric Research)H-Index: 3
view all 0 authors...
#1Veronika Eyring (University of Bremen)H-Index: 48
#2Peter M. Cox (University of Exeter)H-Index: 70
Last.Forrest M. Hoffman (UT: University of Tennessee)H-Index: 33
view all 29 authors...
Earth system models are complex and represent a large number of processes, resulting in a persistent spread across climate projections for a given future scenario. Owing to different model performances against observations and the lack of independence among models, there is now evidence that giving equal weight to each available model projection is suboptimal. This Perspective discusses newly developed tools that facilitate a more rapid and comprehensive evaluation of model simulations with obse...
#1Doug Smith (Met Office)H-Index: 38
#2Adam A. Scaife (University of Exeter)H-Index: 50
Last.Francisco J. Doblas-Reyes (Barcelona Supercomputing Center)H-Index: 9
view all 33 authors...
The Paris Agreement calls for efforts to limit anthropogenic global warming to less than 1.5 °C above preindustrial levels. However, natural internal variability may exacerbate anthropogenic warming to produce temporary excursions above 1.5 °C. Such excursions would not necessarily exceed the Paris Agreement, but would provide a warning that the threshold is being approached. Here we develop a new capability to predict the probability that global temperature will exceed 1.5 °C above preindustria...
#1Gerald A. Meehl (NCAR: National Center for Atmospheric Research)H-Index: 93
#2Christine T. Y. Chung (BOM: Bureau of Meteorology)H-Index: 7
Last.Cecilia M. Bitz (UW: University of Washington)H-Index: 49
view all 5 authors...
#1Yuanlong Li (CU: University of Colorado Boulder)H-Index: 15
#2Weiqing Han (CU: University of Colorado Boulder)H-Index: 33
Last.Fan Wang (CAS: Chinese Academy of Sciences)H-Index: 16
view all 5 authors...
AbstractOcean heat uptake is the primary heat sink of the globe and modulates its surface warming rate. In situ observations during the past half century documented obvious multidecadal variations in the upper-ocean heat content (0–400 m; OHC400) of the Indian Ocean (IO). The observed OHC400 showed an increase of (5.9 ± 2.5) × 1021 J decade−1 during 1965–79, followed by a decrease of (−5.2 ± 2.5) × 1021 J decade−1 during 1980–96, and a rapid increase of (13.6 ± 1.1) × 1021 J decade−1 during 2000...
12345678910