That said, competitors have caught up to SteelSeries in terms of audio quality, offering larger 50mm drivers and more robust digital audio tweaks via software.

Armour, K., Marshall, J., Scott, J., Donohoe, A. & Newsom, E. Southern Ocean warming delayed by circumpolar upwelling and equatorward transport. Nat. Geosci. 9, 549–554 (2016). Previous studies have shown that CO 2-forced GCMs simulate similar advection of lower tropospheric warm anomalies from newly ice-free ocean regions in the Arctic to adjacent land regions: while summer season sea ice decline and ocean mixed layer warming in the Arctic directly cause (delayed) surface-amplified warming over the Arctic Ocean in fall and winter 7, warming over boreal land regions is primarily through warm air advection from the polar oceans 29. Therefore, when Antarctic orography is flattened, there is greater similarity between the poles in how advection of boundary layer air from newly ice-free ocean waters warms land areas in winter. Greater surface-amplified warming with flattened orographyMcGraw, M. & Barnes, E. Seasonal sensitivity of the eddy-driven jet to tropospheric heating in an idealized AGCM. J. Clim. 29, 5223–5240 (2016). GISTEMP spatially extrapolates temperatures into unmeasured regions using a 1200-km radius of influence for the stations. BEST employs kriging-based spatial interpolation, and HadCRUT5 uses their own statistical infilling method. In all these datasets, areas of sea ice are treated as if they were land, and SST observations are used and extrapolated only at the grid cells which are ice free. The coverage of sea ice is obtained from Met Office Hadley Centre sea ice and sea surface temperature data set, HadISST2 65. Walsh, K., Simmonds, I. & Collier, M. Sigma-coordinate calculation of topographically forced baroclinicity around Antarctica. Dyn. Atmos. Ocean. 33, 1–29 (2000). Tedesco, M.; Mote, T.; Fettweis, X.; Hanna, E.; Jeyaratnam, J.; Booth, J. F.; Datta, R.; Briggs, K. (2016). "Arctic cut-off high drives the poleward shift of a new Greenland melting record". Nature Communications. 7: 11723. Bibcode: 2016NatCo...711723T. doi: 10.1038/ncomms11723. PMC 4906163. PMID 27277547. McGhee, Robert (2005). The last imaginary place: a human history of the Arctic world (Digitized 7 October 2008ed.). Oxford University Press. p.55. ISBN 978-0-19-518368-9. Archived from the original on 30 June 2023 . Retrieved 24 August 2020.

Abrupt Climate Change Focus Of U.S. National Laboratories". Science Daily. 23 September 2008. Archived from the original on 23 June 2017 . Retrieved 28 February 2018. Since it is clear that both greater Antarctic amplification and greater CO 2-forced warming over the Antarctic continent with flattened orography are most prominent in winter (JJA), for the remainder of this study we focus on this season, as we analyze the Antarctic continental warming and bring to light the mechanisms responsible for it. Society, National Geographic (6 October 2016). "Arctic". National Geographic Society. Archived from the original on 3 June 2020 . Retrieved 11 June 2020. Screen, J. A. & Simmonds, I. The central role of diminishing sea ice in recent Arctic temperature amplification. Nature 464, 1334–1337 (2010). McCannon, John. A History of the Arctic: Nature, Exploration and Exploitation. Reaktion Books and University of Chicago Press, 2012. ISBN 9781780230184

User reviews

Held, I. & Soden, B. Robust reponses of the hydrological cycle to global warming. J. Clim. 19, 5686–5699 (2006). Seviour, W. et al. The Southern Ocean sea surface temperature response to ozone depletion: a multimodel comparison. J. Clim. 32, 5107–5121 (2019). Manabe, S. & Wetherald, R. The effects of doubling the CO 2 concentration on the climate of a general circulation model. J. Atmos. Sci. 32, 3–15 (1975).

Addison, Kenneth (2002). Fundamentals of the physical environment. Routledge. p.482. ISBN 978-0-415-23293-7. Archived from the original on 30 June 2023 . Retrieved 15 November 2015.

where L v is the latent heat of fusion, q is the specific humidity, C p is the specific heat of dry air at constant pressure, T is the temperature, g is the acceleration due to gravity, and Φ is the height relative to the geoid. When moist isentropes are flatter (as when Antarctic orography is flattened), air parcels gain less geopotential as they flow poleward, and therefore retain more moisture. This is also evident in the change in specific humidity with CO 2-doubling (Fig. 5, colors): the (poleward) gradient of this specific humidity change along a moist isentropic surface, ∇(∆ q) | θE, is greater with present-day Antarctic orography (panels a, c) than with flattened Antarctic orography (panels b, d), indicating that more moisture is lost along this trajectory with present-day orography than with flattened orography (compare, for example, the gradient of the change in specific humidity, denoted by the blue colors, along the 270 K moist isentrope in Fig. 5a, c with those in 5b, d). Salzmann, M. The polar amplification asymmetry: role of Antarctic surface height. Earth Syst. Dyn. 8, 323–336 (2017).

Climate change is also predicted to have a large impact on tundra vegetation, causing an increase of shrubs, [52] and having a negative impact on bryophytes and lichens. [53]Neale, R. B. et al. The mean climate of the Community Atmosphere Model (CAM4) in forced SST and fully coupled experiments. J. Clim. 26, 5150–5168 (2013).