Using CMIP6 Models to Assess Future Climate Change Effects on Mine Sites in Kazakhstan

被引:7
|
作者
Golian, Saeed [1 ]
El-Idrysy, Houcyne [2 ]
Stambuk, Desana [3 ]
机构
[1] SRK Consulting Kazakhstan Ltd, 77 Kunayev St, Pk View Off Tower, 14th Floor, Alma Ata 050010, Kazakhstan
[2] SRK Consulting Kazakhstan Ltd, Head Off, 5th Floor, Churchill House, 17 Churchill Way, Cardiff CF10 2HH, Wales
[3] SRK Consulting UK Ltd, Head Off, 5th Floor, Churchill House, 17 Churchill Way, Cardiff CF10 2HH, Wales
关键词
climate change; SSPs scenarios; water management; mining; Kazakhstan; PRECIPITATION;
D O I
10.3390/hydrology10070150
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Climate change is a threat to mining and other industries, especially those involving water supply and management, by inducing or amplifying some climatic parameters such as changes in precipitation regimes and temperature extremes. Using the latest NASA NEX-GDDP-CMIP6 datasets, this study quantifies the level of climate change that may affect the development of two mine sites (site 1 and site 2) in north-east Kazakhstan. The study analyses the daily precipitation and maximum and minimum temperature a of a number of global circulation models (GCM) over three future time periods, the 2040s, 2060s, and 2080s, under two shared socioeconomic pathway (SSP) scenarios, SSP245 and SSP585, against the baseline period 1981-2014. The analyses reveal that: (1) both maximum and minimum temperature will increase under both SSP in those time periods, with the rate of change for minimum temperature being higher than maximum temperature. Minimum temperature, for example, will increase by 2.2 and 2.7 & DEG;C under SSP245 and SSP585, respectively, over the 2040s period at both sites; (2) the mean annual precipitation will increase by an average rate of 7% and 10.5% in the 2040s for SSP245 and 17.5% and 7.5% for SSP585 in the 2080s at site 1 and site 2, respectively. It is also observed that summer months will experience drier condition whilst all other months will increase in precipitation; (3) the values of 24 h precipitation with a 10 year return period will also increase under both SSP scenarios and future time periods for most of the studied GCM and at both mine sites. For instance, over the near future period, a 6.9% and 2.8% increase in 10 year 24 h precipitation is expected to happen over site 1 and site 2, respectively, under SSP245. These predicted changes should be considered as design criteria adjustments for projected water supply and water management structures.
引用
收藏
页数:13
相关论文
共 50 条
  • [31] Projecting Future Vegetation Change for Northeast China Using CMIP6 Model
    Yuan, Wei
    Wu, Shuang-Ye
    Hou, Shugui
    Xu, Zhiwei
    Pang, Hongxi
    Lu, Huayu
    REMOTE SENSING, 2021, 13 (17)
  • [32] Future Climate Under CMIP6 Solar Activity Scenarios
    Sedlacek, Jan
    Sukhodolov, Timofei
    Egorova, Tania
    Karagodin-Doyennel, Arseniy
    Rozanov, Eugene
    EARTH AND SPACE SCIENCE, 2023, 10 (07)
  • [33] Insights From CMIP6 for Australia's Future Climate
    Grose, M. R.
    Narsey, S.
    Delage, F. P.
    Dowdy, A. J.
    Bador, M.
    Boschat, G.
    Chung, C.
    Kajtar, J. B.
    Rauniyar, S.
    Freund, M. B.
    Lyu, K.
    Rashid, H.
    Zhang, X.
    Wales, S.
    Trenham, C.
    Holbrook, N. J.
    Cowan, T.
    Alexander, L.
    Arblaster, J. M.
    Power, S.
    EARTHS FUTURE, 2020, 8 (05)
  • [34] Assessment of climate change impact on meteorological variables of Indravati River Basin using SDSM and CMIP6 models
    Challa, Venkateswarlu
    Renganathan, Manjula
    ENVIRONMENTAL MONITORING AND ASSESSMENT, 2024, 197 (01)
  • [35] Prediction of the Global Distribution of Arhopalus rusticus under Future Climate Change Scenarios of the CMIP6
    Fan, Yuhang
    Zhang, Xuemei
    Zhou, Yuting
    Zong, Shixiang
    FORESTS, 2024, 15 (06):
  • [36] Time Variability Correction of CMIP6 Climate Change Projections
    Shao, Y.
    Bishop, C. H.
    Hobeichi, S.
    Nishant, N.
    Abramowitz, G.
    Sherwood, S.
    JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS, 2024, 16 (02)
  • [37] CMIP6 multi-model prediction of future climate change in the Hotan River Basin
    He C.
    Luo C.
    Chen F.
    Long A.
    Tang H.
    Earth Science Frontiers, 2023, 30 (03) : 515 - 528
  • [38] Selection and downscaling of CMIP6 climate models in Northern Nigeria
    Wada, Idris Muhammad
    Usman, Haruna Shehu
    Nwankwegu, Amechi S.
    Usman, Makhai Nwunuji
    Gebresellase, Selamawit Haftu
    THEORETICAL AND APPLIED CLIMATOLOGY, 2023, 153 (3-4) : 1157 - 1175
  • [39] The global energy balance as represented in CMIP6 climate models
    Martin Wild
    Climate Dynamics, 2020, 55 : 553 - 577
  • [40] Selection and downscaling of CMIP6 climate models in Northern Nigeria
    Idris Muhammad Wada
    Haruna Shehu Usman
    Amechi S. Nwankwegu
    Makhai Nwunuji Usman
    Selamawit Haftu Gebresellase
    Theoretical and Applied Climatology, 2023, 153 : 1157 - 1175