The poleward migration of the location of tropical cyclone maximum intensity.
about
Marine reserves can mitigate and promote adaptation to climate change.Tropical cyclones in a year of rising global temperatures and a strengthening El Niño.Rapid intensification and the bimodal distribution of tropical cyclone intensityThe broad footprint of climate change from genes to biomes to people.Asymmetric response of tropical cyclone activity to global warming over the North Atlantic and western North Pacific from CMIP5 model projectionsImpacts of increasing typhoons on the structure and function of a subtropical forest: reflections of a changing climate.Extreme rainfall activity in the Australian tropics reflects changes in the El Niño/Southern Oscillation over the last two millenniaRecent decrease in typhoon destructive potential and global warming implicationsThe silent services of the world ocean.Stratified coastal ocean interactions with tropical cyclones.Rainfall-enhanced blooming in typhoon wakesPersistent northward North Atlantic tropical cyclone track migration over the past five centuries.Enhanced intensity of global tropical cyclones during the mid-Pliocene warm period.Impact of Ocean Warming on Tropical Cyclone Size and Its Destructiveness.Human influence on tropical cyclone intensity.Climate science: Shifting storms.Rapid shelf-wide cooling response of a stratified coastal ocean to hurricanes.Impact of climate change on New York City's coastal flood hazard: Increasing flood heights from the preindustrial to 2300 CE.Global warming hiatus contributed to the increased occurrence of intense tropical cyclones in the coastal regions along East Asia.Westward migration of tropical cyclone rapid-intensification over the Northwestern Pacific during short duration El Niño.Tropical cyclones and climate changeNatural hazards in Australia: storms, wind and hailExtreme tropical cyclone activities in the southern Pacific OceanWestern North Pacific Tropical Cyclone Model Tracks in Present and Future ClimatesClimate change impacts in Latin America and the Caribbean and their implications for developmentVariations in the power dissipation index in the East Asia regionImpact of ocean warming on tropical cyclone track over the western north pacific: A numerical investigation based on two case studiesIs the poleward migration of tropical cyclone maximum intensity associated with a poleward migration of tropical cyclone genesis?Relationships between Ambient Ozone Concentration Changes in Southwestern Taiwan and Invasion Tracks of Tropical TyphoonsLatitudinal Change of Tropical Cyclone Maximum Intensity in the Western North PacificLong-term trends of typhoon-induced rainfall over Taiwan: In situ evidence of poleward shift of typhoons in western North Pacific in recent decades
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P2860
The poleward migration of the location of tropical cyclone maximum intensity.
description
2014 nî lūn-bûn
@nan
2014年の論文
@ja
2014年論文
@yue
2014年論文
@zh-hant
2014年論文
@zh-hk
2014年論文
@zh-mo
2014年論文
@zh-tw
2014年论文
@wuu
2014年论文
@zh
2014年论文
@zh-cn
name
The poleward migration of the location of tropical cyclone maximum intensity.
@en
The poleward migration of the location of tropical cyclone maximum intensity.
@nl
type
label
The poleward migration of the location of tropical cyclone maximum intensity.
@en
The poleward migration of the location of tropical cyclone maximum intensity.
@nl
prefLabel
The poleward migration of the location of tropical cyclone maximum intensity.
@en
The poleward migration of the location of tropical cyclone maximum intensity.
@nl
P2860
P356
P1433
P1476
The poleward migration of the location of tropical cyclone maximum intensity.
@en
P2093
Kerry A Emanuel
P2860
P2888
P304
P356
10.1038/NATURE13278
P407
P577
2014-05-01T00:00:00Z
P5875
P6179
1008190755