Brief communication: CMIP6 does not suggest any atmospheric blocking increase in summer over Greenland by 2100

• Published in: International Journal of Climatology
• Main Authors: Delhasse, Alison, Hanna, E., Kittel, Christoph, Fettweis, Xavier
• Other Authors: Sphères - SPHERES
• Format: Article in Journal/Newspaper
• Language: English
• Published: John Wiley & Sons 2021
• Subjects: Physical; chemical; mathematical & earth Sciences; Earth sciences & physical geography; Physique; chimie; mathématiques & sciences de la terre; Sciences de la terre & géographie physique; Greenland; Ice Sheet
• Online Access: https://orbi.uliege.be/handle/2268/254965; https://orbi.uliege.be/bitstream/2268/254965/1/Delhasse-2020-Int.%20Journal%20%28GRD%2cCMIP6%2ccirculation%29.pdf; https://doi.org/10.1002/joc.6977

peer reviewed The Greenland blocking index (GBI), an indicator of the synoptic‐scale circulation over Greenland, has been anomalously positive during most summers since the late 1990s. Such changes in atmospheric circulation, favouring anticyclonic conditions, have led to an increase in Greenland summer temperatures, a decrease in cloud cover and larger surface melt. The GBI is therefore a key indicator of melting and surface mass balance variability over the Greenland ice sheet. However, the models of fifth phase of the Coupled Model Intercomparison Project (CMIP5) do not represent the increase in GBI that is suggested by recent observations, and do not project any significant increase in GBI until 2100. In this study, the new generation of CMIP6 Earth‐system models is evaluated in order to analyse the evolution of the future GBI. All CMIP5 and CMIP6 projections reveal the same trend towards a decrease of the GBI until 2100 and no model reproduces the strong increase in the persistence of summer blocking events observed over the last few decades. Significant melting events related to a highly positive GBI, as observed in summer 2019, are still not considered by CMIP6 models and therefore the projected surface melt increase of the ice sheet could be underestimated if such summer circulation changes persist in the next decades. This research has been supported by F.R.S.‐FNRS, the Fonds Wetenschappelijk Onderzoek‐Vlaanderen (FWO) under the EOS project no. O0100718F and the European Union's Horizon 2020 research and innovation programme under the PROTECT project no. 869304. This is PROTECT contribution number 7.