Hydroclimate in a Changing World: Recent Trends, Current Progress and Future Directions
Global warming is imposing tremendous challenges upon human and otherwise biotic life on Earth. A warmer atmosphere holds more moisture. The consensus is that the moisture transport by the atmospheric circulation strengthens and makes already wet areas of moisture convergence wetter and already dry...
Format: | eBook |
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Language: | English |
Published: |
Basel
MDPI - Multidisciplinary Digital Publishing Institute
2023
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Online Access: | Open Access: DOAB: description of the publication Open Access: DOAB, download the publication |
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720 | 1 | |a Liu, Haibo |4 edt | |
720 | 1 | |a Liu, Haibo |4 oth | |
245 | 0 | 0 | |a Hydroclimate in a Changing World: Recent Trends, Current Progress and Future Directions |
260 | |a Basel |b MDPI - Multidisciplinary Digital Publishing Institute |c 2023 | ||
300 | |a 1 online resource (250 p.) | ||
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506 | 0 | |a Open Access |f Unrestricted online access |2 star | |
520 | |a Global warming is imposing tremendous challenges upon human and otherwise biotic life on Earth. A warmer atmosphere holds more moisture. The consensus is that the moisture transport by the atmospheric circulation strengthens and makes already wet areas of moisture convergence wetter and already dry areas of moisture divergence drier. Therefore, the tropics and mid-to-high latitudes will get wetter and the subtropics will get drier. Without any change in the interannual variability of hydroclimate, the change in the mean hydroclimate would equally increase drought risk in some places and flood risk in others. Moreover, global warming will cause the interannual variability of the hydroclimate to intensify, which will induce more droughts and floods. Furthermore, the changing atmospheric circulation interaction with the land surface may cause storm track alterations and may play an important role in shaping moisture redistribution. The author's contributions have documented the precipitation trends in southeast of the US, the Nile River Basin Ethiopia, Iraq, the Huai River Basin of northern China, and the Qilian Mountains of western China. The precipitation predictability on both global and regional scales are also studied. The interaction among climate systems in southeast Asia is also explicitly documented. | ||
540 | |a Creative Commons |f https://creativecommons.org/licenses/by/4.0/ |2 cc |u https://creativecommons.org/licenses/by/4.0/ | ||
546 | |a English | ||
650 | 7 | |a Meteorology & climatology |2 bicssc | |
650 | 7 | |a Research & information: general |2 bicssc | |
653 | |a atmospheric circulation | ||
653 | |a Bayesian Ensemble Algorithm | ||
653 | |a central Punjab | ||
653 | |a CHIRPS | ||
653 | |a climate change | ||
653 | |a climate projection | ||
653 | |a climate trend | ||
653 | |a CMIP5 | ||
653 | |a CMIP6 | ||
653 | |a consistency | ||
653 | |a cyclones power dissipation index (PDI) | ||
653 | |a descriptive statistics | ||
653 | |a drought index | ||
653 | |a dynamic Z-I | ||
653 | |a El Niño | ||
653 | |a El Niño southern oscillation (ENSO) | ||
653 | |a ENSO | ||
653 | |a flood magnitude | ||
653 | |a global | ||
653 | |a Google Earth Engine | ||
653 | |a groundwater levels | ||
653 | |a Huai River Basin | ||
653 | |a Indian Ocean dipole (IOD) | ||
653 | |a interannual and long-term trend | ||
653 | |a Iraq | ||
653 | |a land cover/land use | ||
653 | |a land use land cover | ||
653 | |a Loess Plateau | ||
653 | |a LSTM neural network | ||
653 | |a Mann-Kendall test | ||
653 | |a MJO | ||
653 | |a monsoon trough | ||
653 | |a n/a | ||
653 | |a NDVI | ||
653 | |a Nile River Basin | ||
653 | |a non-parametric trends | ||
653 | |a PERSIANN-CDR | ||
653 | |a precipitable water | ||
653 | |a precipitation | ||
653 | |a precipitation estimation | ||
653 | |a predictability | ||
653 | |a Qilian Mountains | ||
653 | |a radar | ||
653 | |a raindrop spectrum | ||
653 | |a rainfall | ||
653 | |a rainfall change | ||
653 | |a rainstorm and flood | ||
653 | |a rainstorm intensity | ||
653 | |a rainstorm process | ||
653 | |a relative soil moisture | ||
653 | |a risk estimation and mapping | ||
653 | |a risk prediction | ||
653 | |a seasonal precipitation | ||
653 | |a Southwest China | ||
653 | |a spatial and temporal change | ||
653 | |a spring maize | ||
653 | |a surface water vapor pressure | ||
653 | |a temperature | ||
653 | |a trend analysis | ||
653 | |a trends and variability | ||
653 | |a vegetation | ||
653 | |a Walker circulation | ||
653 | |a water resources | ||
653 | |a winter weather types | ||
793 | 0 | |a DOAB Library. | |
856 | 4 | 0 | |u https://directory.doabooks.org/handle/20.500.12854/132440 |7 0 |z Open Access: DOAB: description of the publication |
856 | 4 | 0 | |u https://mdpi.com/books/pdfview/book/8478 |7 0 |z Open Access: DOAB, download the publication |