Downscaling CMIP5 climate models shows increased tropical cyclone activity over the 21st century
about
Robust Performance of Marginal Pacific Coral Reef Habitats in Future Climate ScenariosThe intertropical convergence zone modulates intense hurricane strikes on the western North Atlantic marginFemale hurricanes are deadlier than male hurricanesLong-term changes in Australian tropical cyclone numbersTracking the Evolution of Infrastructure Systems and Mass Responses Using Publically Available DataA review on regional convection-permitting climate modeling: Demonstrations, prospects, and challenges.Barrier island morphology and sediment characteristics affect the recovery of dune building grasses following storm-induced overwash.Model projections of atmospheric steering of Sandy-like superstorms.Operationalizing resilience for adaptive coral reef management under global environmental change.Typhoon Yolanda/Haiyan and climate justice.New York City Panel on Climate Change 2015 Report. Chapter 2: Sea level rise and coastal storms.Coastal foredune evolution: the relative influence of vegetation and sand supply in the US Pacific Northwest.Flood Risk, Flood Mitigation, and Location Choice: Evaluating the National Flood Insurance Program's Community Rating System.Hurricane Sandy's flood frequency increasing from year 1800 to 2100.The 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 projectionsThe threat to coral reefs from more intense cyclones under climate change.Projected changes in African easterly wave intensity and track in response to greenhouse forcing.Extreme rainfall activity in the Australian tropics reflects changes in the El Niño/Southern Oscillation over the last two millenniaTree Rings Show Recent High Summer-Autumn Precipitation in Northwest Australia Is Unprecedented within the Last Two Centuries.Recent decrease in typhoon destructive potential and global warming implicationsChange in ocean subsurface environment to suppress tropical cyclone intensification under global warming.Atlantic hurricane surge response to geoengineering.Tropical cyclone activity enhanced by Sahara greening and reduced dust emissions during the African Humid Period.Inner Workings: Exploring ancient storms in marshes, corals, and caves.Observational evidence supports the role of tropical cyclones in regulating climate.Rainfall-enhanced blooming in typhoon wakesHuman influence on tropical cyclone intensity.Quantifying the severity of hurricanes on extinction probabilities of a primate population: Insights into "Island" extirpations.Nutrient enrichment intensifies hurricane impact in scrub mangrove ecosystems in the Indian River Lagoon, Florida, USA.Impacts of hemispheric solar geoengineering on tropical cyclone frequency.Cultural Variability in the Link Between Environmental Concern and Support for Environmental Action.Estimating economic damage from climate change in the United States.Assessing the present and future probability of Hurricane Harvey's rainfall.Impact of climate change on New York City's coastal flood hazard: Increasing flood heights from the preindustrial to 2300 CE.Barrier island bistability induced by biophysical interactionsA state-space modelling approach to wildlife monitoring with application to flying-fox abundance.Effects of sandfish (Holothuria scabra) removal on shallow-water sediments in Fiji.Ecosystem‐based management of coral reefs under climate change.Stability and bistability in a one-dimensional model of coastal foredune height
P2860
Q28547997-EAA6A578-542C-44C9-A29C-C04BC5999F21Q28603857-AAFBBE7C-20E2-42E7-9D93-4502B67E9596Q28657814-6C2B1D6E-C85D-4BAE-A7CE-E245E6F1D593Q29400292-DFF44FA3-6050-4852-854F-B4FB1128CF3CQ30000295-948B1F5B-4429-4018-A25D-A5838B36A624Q30378117-50769480-B957-4723-BA31-5305BD6FF6BDQ30411187-47D940C6-66DD-4A68-BEF7-6E17DB749293Q30664873-73D675CA-D282-404B-8254-CDF72C110531Q30848044-17C30213-B720-4389-A3B5-8017EE534E83Q30859815-CEB17A67-ABB1-4696-A895-A8E6FBA94FC3Q30894282-C2A4E71B-EC8E-4D9C-B495-781A51F7DC4EQ30921481-A0FF0DD2-8F8F-4F3A-95BF-318B2FA3BC21Q31020493-40680962-B42D-40ED-A939-8D8520F6005FQ31139668-5A61C3A6-43AB-401E-8836-97C344E8F448Q31142453-CFD597C7-F05B-478E-A790-123720F3498CQ31157730-9E500498-CF29-4E6B-93D4-D4BFCEBFC182Q31158030-AB1678DD-3EE1-48E6-9089-A7251E0601BBQ33627445-FDA1F0C1-F03C-4766-8E81-96FA6B575FF0Q35485231-8C8612F9-E4B6-4B75-987B-61CF0F8E2715Q35651159-8C8659AE-1476-47F3-9910-6A35C554F8ACQ35681842-1B75EC65-0700-4A3B-8406-F5BE73A8BAA7Q35775426-54006F78-0DCB-4809-AB25-CDBFB602A2AFQ36300164-EDAD8B7C-E1A4-42AB-91A1-0857249E0CC6Q36385508-67FAD14B-5C4F-4996-A7DE-18B151375BEAQ36742657-8264F718-A5CB-4E52-AED3-B3B7A2D5E19FQ37191999-2A7D085F-846C-473D-B215-0543DE08521EQ37193153-09A15C18-E862-447F-A16D-8751FBC05227Q38841694-3C69AE2D-6421-42BB-80E8-734941FD042EQ38872434-8937429F-AB4E-446E-9274-15BE2A721722Q39001780-65B42875-0A53-48C4-8499-332D771DD07CQ43528131-EF57CF46-EF56-47F4-BA33-C02BC49B5CFDQ44410301-5773FDB0-AF6F-466B-8054-6F389BE78DDEQ45370590-FB981493-0D13-4527-949A-9667712A059EQ47132456-5CD86CC6-A837-4DD6-B05D-6BE4D39B641BQ47141615-E074263A-273D-41EC-85E0-3B02B5A30A40Q54246801-CC36462D-CF4F-440E-B208-39B5209EF4F1Q54957600-83B6B35A-6C93-441D-BEB8-B5F001BC9FD6Q55155585-222E7032-5BC2-45E5-B469-78AB6D63BAE8Q55501677-70D1398D-3362-47D2-90A6-69F405790733Q56041337-79C11C57-3B33-4722-836B-66115DA0B168
P2860
Downscaling CMIP5 climate models shows increased tropical cyclone activity over the 21st century
description
2013 nî lūn-bûn
@nan
2013 թուականի Յուլիսին հրատարակուած գիտական յօդուած
@hyw
2013 թվականի հուլիսին հրատարակված գիտական հոդված
@hy
2013年の論文
@ja
2013年論文
@yue
2013年論文
@zh-hant
2013年論文
@zh-hk
2013年論文
@zh-mo
2013年論文
@zh-tw
2013年论文
@wuu
name
Downscaling CMIP5 climate mode ...... activity over the 21st century
@ast
Downscaling CMIP5 climate mode ...... activity over the 21st century
@en
Downscaling CMIP5 climate mode ...... activity over the 21st century
@nl
type
label
Downscaling CMIP5 climate mode ...... activity over the 21st century
@ast
Downscaling CMIP5 climate mode ...... activity over the 21st century
@en
Downscaling CMIP5 climate mode ...... activity over the 21st century
@nl
prefLabel
Downscaling CMIP5 climate mode ...... activity over the 21st century
@ast
Downscaling CMIP5 climate mode ...... activity over the 21st century
@en
Downscaling CMIP5 climate mode ...... activity over the 21st century
@nl
P356
P1476
Downscaling CMIP5 climate mode ...... activity over the 21st century
@en
P2093
Kerry A Emanuel
P2860
P304
12219-12224
P356
10.1073/PNAS.1301293110
P407
P577
2013-07-08T00:00:00Z