Matches in SemOpenAlex for { <https://semopenalex.org/work/W4229372271> ?p ?o ?g. }
- W4229372271 endingPage "3416" @default.
- W4229372271 startingPage "3395" @default.
- W4229372271 abstract "The extreme temperature has become more frequent and intense due to global warming, particularly in dry regions, causing devastating impacts on humans and ecosystems. The transboundary Amu river basin (ARB) is the most vulnerable region in Central Asia (CA) to extreme weather linked to climate change. This study aimed to project warm and cold extremes in ARB for four Shared Socioeconomic Pathways (SSP1-2.6, SSP2-4.5, SSP3-7.0 and SSP5-8.5) and two time-horizons, 2020–2059 and 2060–2099, using daily maximum (Tmax) and minimum temperature (Tmin) simulations of global climate models (GCMs) of Coupled Model Inter-comparison Project phase six (CMIP6). Results revealed that the basin’s west experiences more hot extremes and the east more cold extremes. Climate change would cause a significant increase in the annual mean of Tmax and Tmin. However, the increase in mean Tmin would be much higher (5.0ºC ) than the mean Tmax (4.6ºC ). It would cause an increase in the hot extremes and a decrease in the cold extremes in the basin. The higher increase in the hot extremes would be in the west, while the higher decrease in the cold extreme in the basin’s east. The number of days above 40℃ would increase from 45 to 60 days in the basin’s west and northwest compared to the historical period. The number of days below − 20℃ would decrease up to 45 days in the basin’s east. Overall, the decrease in cold extremes would be much faster than the increase in hot extremes." @default.
- W4229372271 created "2022-05-10" @default.
- W4229372271 creator A5023212489 @default.
- W4229372271 creator A5041901750 @default.
- W4229372271 creator A5048455026 @default.
- W4229372271 creator A5057749312 @default.
- W4229372271 creator A5059837862 @default.
- W4229372271 date "2022-05-09" @default.
- W4229372271 modified "2023-10-11" @default.
- W4229372271 title "Projection of Hot and Cold Extremes in the Amu River Basin of Central Asia using GCMs CMIP6" @default.
- W4229372271 cites W1539419152 @default.
- W4229372271 cites W1914321236 @default.
- W4229372271 cites W1964308073 @default.
- W4229372271 cites W1991308688 @default.
- W4229372271 cites W2003002154 @default.
- W4229372271 cites W2021530952 @default.
- W4229372271 cites W2092017495 @default.
- W4229372271 cites W2167458864 @default.
- W4229372271 cites W2193503481 @default.
- W4229372271 cites W2197490289 @default.
- W4229372271 cites W2294046870 @default.
- W4229372271 cites W2377071656 @default.
- W4229372271 cites W2413934019 @default.
- W4229372271 cites W2750204209 @default.
- W4229372271 cites W2779715464 @default.
- W4229372271 cites W2806127995 @default.
- W4229372271 cites W2807236430 @default.
- W4229372271 cites W2836147354 @default.
- W4229372271 cites W2885747415 @default.
- W4229372271 cites W2888603611 @default.
- W4229372271 cites W2900335298 @default.
- W4229372271 cites W2904516924 @default.
- W4229372271 cites W2911859640 @default.
- W4229372271 cites W2929484919 @default.
- W4229372271 cites W2944495903 @default.
- W4229372271 cites W2950658079 @default.
- W4229372271 cites W2956255334 @default.
- W4229372271 cites W2980644126 @default.
- W4229372271 cites W2981218717 @default.
- W4229372271 cites W2989005980 @default.
- W4229372271 cites W2995378905 @default.
- W4229372271 cites W2997329188 @default.
- W4229372271 cites W3003857487 @default.
- W4229372271 cites W3005182449 @default.
- W4229372271 cites W3007479447 @default.
- W4229372271 cites W3012106770 @default.
- W4229372271 cites W3022143763 @default.
- W4229372271 cites W3029509436 @default.
- W4229372271 cites W3030832731 @default.
- W4229372271 cites W3036082713 @default.
- W4229372271 cites W3036643635 @default.
- W4229372271 cites W3037499694 @default.
- W4229372271 cites W3040167408 @default.
- W4229372271 cites W3046984087 @default.
- W4229372271 cites W3048501727 @default.
- W4229372271 cites W3092633457 @default.
- W4229372271 cites W3094171817 @default.
- W4229372271 cites W3094836545 @default.
- W4229372271 cites W3097295640 @default.
- W4229372271 cites W3099011099 @default.
- W4229372271 cites W3108729183 @default.
- W4229372271 cites W3113434477 @default.
- W4229372271 cites W3121914409 @default.
- W4229372271 cites W3122281830 @default.
- W4229372271 cites W3124307135 @default.
- W4229372271 cites W3139006845 @default.
- W4229372271 cites W3146215885 @default.
- W4229372271 cites W3148250422 @default.
- W4229372271 cites W3153249002 @default.
- W4229372271 cites W3161696442 @default.
- W4229372271 cites W3163060798 @default.
- W4229372271 cites W3167033635 @default.
- W4229372271 cites W3169308145 @default.
- W4229372271 cites W3178824006 @default.
- W4229372271 cites W3181205698 @default.
- W4229372271 cites W3193536156 @default.
- W4229372271 cites W3195663516 @default.
- W4229372271 cites W3198231277 @default.
- W4229372271 cites W3198500275 @default.
- W4229372271 cites W3203733310 @default.
- W4229372271 cites W3204847850 @default.
- W4229372271 cites W3209515246 @default.
- W4229372271 cites W3211499667 @default.
- W4229372271 cites W3215076901 @default.
- W4229372271 cites W4200028515 @default.
- W4229372271 cites W4200043061 @default.
- W4229372271 cites W4206588006 @default.
- W4229372271 doi "https://doi.org/10.1007/s00477-022-02201-6" @default.
- W4229372271 hasPublicationYear "2022" @default.
- W4229372271 type Work @default.
- W4229372271 citedByCount "15" @default.
- W4229372271 countsByYear W42293722712022 @default.
- W4229372271 countsByYear W42293722712023 @default.
- W4229372271 crossrefType "journal-article" @default.
- W4229372271 hasAuthorship W4229372271A5023212489 @default.
- W4229372271 hasAuthorship W4229372271A5041901750 @default.
- W4229372271 hasAuthorship W4229372271A5048455026 @default.
- W4229372271 hasAuthorship W4229372271A5057749312 @default.