J Geophys Res Atmos — Nature — Cannon AJ Multivariate bias correction of climate model output: Matching marginal distributions and intervariable dependence structure. J Clim — Cannon AJ Multivariate quantile mapping bias correction: an N-dimensional probability density function transform for climate model simulations of multiple variables.
Clim Dyn — Sci Rep — Glob Planet Change — Sci Bull — Cheng Q, Zhong F, Wang P Potential linkages of extreme climate events with vegetation and large-scale circulation indices in an endorheic river basin in northwest China.
Atmos Res Int J Climatol — Dai A Increasing drought under global warming in observations and models. Nat Clim Chang — Atmos Res — Duan W, He B, Takara K et al Changes of precipitation amounts and extremes over Japan between and and their connection to climate indices. Duan W, Hanasaki N, Shiogama H et al Evaluation and future projection of Chinese precipitation extremes using large ensemble high-resolution climate simulations. Accessed 5 Apr Fan J, Wu L, Zhang F et al Climate change effects on reference crop evapotranspiration across different climatic zones of China during — J Hydrol — Nat Geosci — Clim Res — In: Clim.
Carbon Br. Accessed 5 Feb Adv Clim Change Res — Cambridge University Press, Cambridge. Google Scholar. Theor Appl Climatol — Kay A Operational amplifier noise. Kendall MG Rank correlation methods, 4th edn. Charles Grifin, London. Clim Change — Eos washington DC — Lin L, Gao T, Luo M et al Contribution of urbanization to the changes in extreme climate events in urban agglomerations across China.
Sci Total Environ J Clean Prod Mann HB Non-parametric test against trend. Econometrica — Papalexiou SM, Montanari A Global and regional increase of precipitation extremes under global warming. Historically, Earth's climate has regularly shifted between temperatures like those we see today and temperatures cold enough to cover much of North America and Europe with ice. The difference between average global temperatures today and during those ice ages is only about 9 degrees Fahrenheit 5 degrees Celsius , and the swings have tended to happen slowly, over hundreds of thousands of years.
But with concentrations of greenhouse gases rising, Earth's remaining ice sheets such as Greenland and Antarctica are starting to melt too. That extra water could raise sea levels significantly, and quickly. By , sea levels are predicted to rise between one and 2. As the mercury rises, the climate can change in unexpected ways. In addition to sea levels rising, weather can become more extreme. This means more intense major storms, more rain followed by longer and drier droughts—a challenge for growing crops—changes in the ranges in which plants and animals can live, and loss of water supplies that have historically come from glaciers.
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Jump to Page. Search inside document. Melting glaciers, early snowmelt, and severe droughts -Melting glaciers, early snowmelt, and severe droughts will cause more dramatic water shortages and increase the risk Result of of wildfires.
Rising sea levels -Rising sea levels will result in floods especially in coastal Global areas. Agriculture and fisheries will be harmed or destroyed as a Enviroment result of all of these issues. Heatwaves -Long durations of extremely high temperatures can be dangerous warming to to the health of vulnerable populations including the elderly and sick. Loss of agricultural productivity -Global warming can result in droughts that can worsen living human health conditions, especially in Africa.
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