LEADER 04059nam 2200901z- 450 001 9910576881703321 005 20220621 035 $a(CKB)5720000000008358 035 $a(oapen)https://directory.doabooks.org/handle/20.500.12854/84424 035 $a(oapen)doab84424 035 $a(EXLCZ)995720000000008358 100 $a20202206d2022 |y 0 101 0 $aeng 135 $aurmn|---annan 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 00$aEnergy and Water Cycles in the Third Pole 210 $aBasel$cMDPI - Multidisciplinary Digital Publishing Institute$d2022 215 $a1 online resource (218 p.) 311 08$a3-0365-3928-X 311 08$a3-0365-3927-1 330 $aAs the most prominent and complicated terrain on the globe, the Tibetan Plateau (TP) is often called the "Roof of the World", "Third Pole" or "Asian Water Tower". The energy and water cycles in the Third Pole have great impacts on the atmospheric circulation, Asian monsoon system and global climate change. On the other hand, the TP and the surrounding higher elevation area are also experiencing evident and rapid environmental changes under the background of global warming. As the headwater area of major rivers in Asia, the TP's environmental changes-such as glacial retreat, snow melting, lake expanding and permafrost degradation-pose potential long-term threats to water resources of the local and surrounding regions. To promote quantitative understanding of energy and water cycles of the TP, several field campaigns, including GAME/Tibet, CAMP/Tibet and TORP, have been carried out. A large amount of data have been collected to gain a better understanding of the atmospheric boundary layer structure, turbulent heat fluxes and their coupling with atmospheric circulation and hydrological processes. The focus of this reprint is to present recent advances in quantifying land-atmosphere interactions, the water cycle and its components, energy balance components, climate change and hydrological feedbacks by in situ measurements, remote sensing or numerical modelling approaches in the "Third Pole" region. 606 $aMeteorology & climatology$2bicssc 606 $aResearch & information: general$2bicssc 610 $aChina 610 $aclimate warming 610 $aconvection-permitting modeling 610 $adriving factors 610 $aEast Asia climate 610 $aelevation-dependency 610 $aET 610 $afull-Stokes model 610 $aglacier modeling 610 $aheat exchange 610 $aHYSPLIT_v4 model 610 $ai-PFASs 610 $aIndian Ocean 610 $alake 610 $alake ice phenology 610 $alake surface temperature 610 $aland-atmosphere interaction 610 $amass balance 610 $amonsoon season 610 $an/a 610 $anon-monsoon season 610 $aobservation data 610 $aprecipitation 610 $aQinghai Province 610 $aradiation fluxes 610 $ariver 610 $arunoff 610 $aSichuan Basin 610 $asingular value decomposition 610 $asummer precipitation 610 $asurface characteristic parameter 610 $asurface fluxes 610 $aterrestrial evapotranspiration 610 $athe Tibetan Plateau 610 $athree river source region 610 $aTibetan Plateau 610 $avertical motion of air 610 $awater resource variation 610 $awater vapor budget 610 $awater vapor transport 610 $aWRF-Hydro model 615 7$aMeteorology & climatology 615 7$aResearch & information: general 700 $aMa$b Yaoming$4edt$01327839 702 $aSu$b Zhongbo$4edt 702 $aZhong$b Lei$4edt 702 $aMa$b Yaoming$4oth 702 $aSu$b Zhongbo$4oth 702 $aZhong$b Lei$4oth 906 $aBOOK 912 $a9910576881703321 996 $aEnergy and Water Cycles in the Third Pole$93038166 997 $aUNINA