被动微波反演土壤水分的L波段新发展及未来展望
赵天杰

Recent advances of L-band application in the passive microwave remote sensing of soil moisture and its prospects
Tianjie ZHAO
表1 适用于L波段的土壤粗糙度参数化方案及其默认参数设置(受权引用自Peng et al, 2017)
Tab.1 Soil roughness parameterization schemes in L-band (from Peng et al, 2017)
类别 名称 参数化方案 参数设置 文献
基于试验数据 C79 rs,p=Γs,hHp
Hp=exp-hcosNp(θi)
h=2)2, Np=2 Choudhury等(1979)
W83 h=2)2, Np=0 Wang等(1983)
W01 h=1.3972m0.5879, Np=0, m=σLc Wigneron等(2001)
W01sm h=0.5761ws-0.3475m0.4230, Np=0, m=σLc Wigneron等(2001)
E07 h=2)2, Np=1 p=h-1 p=v Escorihuela等(2007)
E07sm Np=2)2-4.4ws-wFC,ifwswFC2)2, ifwswFC, Np=1 p=h-1 p=v Escorihuela等(2007)
W11 h=0.9437σ0.8865σ+2.29136, Np=0 Wigneron等(2011)
SMOS h=0.10, if wswt0.10-0.05(ws-wt)wFC-wt, if wtwswFC0.05, if wswFC,
Np=1 p=h-1 p=v
Kerr等(2012)
W99 rs,h=Γs,hHh
rs,v=rs,hcosNθi
Hh=exp -h0.1cosθi
h=, N=0.655, forθi60 Wegmuller等(1999)
S06 rs,h=Γs,hHp
Hp=exp (-h?G(εr,θi,p))
h=σλ22,
G(εr,θi,p)=a-2(εr,θi,p),
a(εr,θi,p)=k1θi,p+k2θi,pεr
Schwank等(2006)
L13 rs,p=1-QΓs,p+QΓs,qHp
Hp=exp -hcosNp(Qi)
h=2.2651-exp-Zs2.023,Zs1.2531.046,Zs>1.253 , Zs=σ2Lc
Q=0.253h, Nv=0.999h-0.54, Nh=Nv+?N
?N=2.029-0.7457Zs
Lawrence等(2013)
G14 Tbp=Ts,eff+aeff,pTa-Ts,eff+rs,p(TbDN-Ts,eff)
rs,p=1-Q)Γs,pGp+QΓs,qGq
aeff,p=1-QAs,p+QAs,Q
Gp=exp-δR2(c0+c1Γs,p)cosc2 (θi)103
Q=0.51.0-sin (2βR)2βR)
As,p=1.0-exp-δR1.5(c3+c4Γs,p)cosc5 (θi)102
Goodberlet等(2014)
基于理论模型 S02 rs,p=Γs,p?exp-22csoθi2+ApΓs,pBp AporBp=exp aθi,p,ρ+bθi,p,ρ?log+cθi,p,ρ?+dθi,p,ρ?W
a,b,c,dθi,p,ρ=ep,ρ+gp,ρθi+h(p,ρ)θi2
Shi等(2002)
C10 rs,p=ApmBpΓs,p Ap,Bp,Cp=apθi3+bpθi2+cpθi+dp ,
m=σLc
Chen等(2010)
Z15 rs,p=Γs,pHp
Hp=Apexp (BpZs2+CpZs)
Ap,Bp,Cp=apθi2+bpθi+cp,
Zs=σ2Lc
Zhao, Shi et al. (2015b)