分窗法估计海表温度函数的系数特征

R. Yokoyama, S. Tanba, T. Watanabe
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The assertion was confirmed by t h e simulation by using Mutsu Bay match-up d a t a set. 1 I \" X 1 0 N The split-window method is known as an excellent algorithm f o r the correct ion of t h e atmospheric e f f e c t s in t h e sea s u r f a c e tempera ture (SST) estimation. Ch. 4 and ch. 5 of AVHRR occupy t h e ad jacent thermal in f ra red bands in t h e atmospheric window. The SST i s es t imated by a l inear function of those br ightness temperatures . For t h e purpose, two typical s t r u c t u r e s have been used, i. e., DVF (dcuble variable function): Y = cX4 bX5 + a SWF (split-window functicn) : = ( c b ) X ~ + b(X4-X.) + a Y = X 4 + g ( x 4 X ~ ) + d where Y i s t h e estimated SST, and X I and X 5 are t h e brightness tempera tures of ch. 4 and ch. 5, respectively. The s t r u c t u r e of SWF comes f rom t h e anlysis to t h e rad ia t ive t r a n s f e r equation. That is, t h e re lat ion between ( Y x , ) and ( X 4 X 5 ) can be approximated to be linear (Maclain 1981. McMillin and Crosby 1984) . Y i s meant t h e s e a t r u t h SST. There are o t h e r dis turbances in t h e SST estimation. Then DVF is introduced as a generalized s t r u c t u r e of SWF. Both DVF and SWF are linear functions, bu t they have d i f fe ren t degrees of freedom in the coefficients. DVF has of two f o r b and c. but SWF has of one f o r g only. The higher degree of freedom can be more flexible t o compensate collaborating e r r o r s totally. The coeff ic ients of SST estimation funct ions a r e usually calculated by applying the regression analysis t o match-up sets of Y. X 4 and X 5 observed direct ly o r indirectly. Table I is a l is t of SST estimation functions proposed by various authors . Both DVF and SWF exis t in the list , but i t is very interest ing that the var iat ions of the i r coeff ic ients remain v e r y small. That is. (1 ) ( c b ) remains near ly eqlual t o one, (2) b and g are r e s t r i c t e d in a narrow range, and (3) a and d are r e s t r i c t e d in a narrow range. Those s imilar i t ies have been understood as a supplementary proof of t h e e f fec t iveness of t h e split-window method (McMillin and Crosby 1 9 8 4 ) . 2 (XIEFFcms WE To m m m ANALYSIS Asaune that a set of mat&-ups IS = { ( Y , , x4 ,. xs d I i l l -NI i s given, where y , , x 4 , and x5 , are observed values of Y , X I and X 5 at a c e r t a i n point and time. i i s the identification number and N is the total number of the match-ups. For general var iables of V and W. descr ibe t h e covariance and t h e cor re la t ion coeff ic ient of them as SV w and RV W . respectively. But f o r t h e convenience, t h e descriptions will be abbreviated as follows. Sx4.x4 4 S . 4 . S X 5 . X S 4 s 5 5 , su Y 4 s w , s x 4 .x5 4 s4 5 . su. x 4 4 s u 4 , s u x 5 4 sus, R x 4 .x5 4 R 4 s . R y . x 4 4 Rv4 , R u . x 5 4 R u 5 The next formulas are obviious f rom t h e s ta t i s t ica l theory. S45 = R 4 5 E X E , Sv4 = R u 4 / X X T , ( 1 )","PeriodicalId":441591,"journal":{"name":"[Proceedings] IGARSS '92 International Geoscience and Remote Sensing Symposium","volume":"2022 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1992-05-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"On the characteristics of Coefficients in SST Estimation Functions by Split-Window Method\",\"authors\":\"R. Yokoyama, S. Tanba, T. Watanabe\",\"doi\":\"10.1109/IGARSS.1992.578484\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"In t h e sea s u r f a c e temperature (SST) estimation by t h e window method f o r AVHRR da ta , two kinds of s t r u c t u r e are popularly assumed in t h e regression analysis. DVF: Y = (c-b)X4 + b(X4-X5) + a SWF: Y = X 4 + g ( x 4 X ~ ) + d where Y , X 4 and X 5 are t h e est imated SST. t h e br ightness tanmatures of ch. 4 and ch. 5 , respectively. The degree of freedom in the coeff ic ient of DVF is two, bu t t h a t of SWF is one. In many empirical resu l t s , however, DVF has similar coeff ic ients t o those in SWF. In th i s paper, t h e s imilar i ty of coeff ic ients i s investigated and showed t h a t i t comes from t h e specif ic charac te r i s t ics of t h e d a t a set provided by t h e split-windows. The assertion was confirmed by t h e simulation by using Mutsu Bay match-up d a t a set. 1 I \\\" X 1 0 N The split-window method is known as an excellent algorithm f o r the correct ion of t h e atmospheric e f f e c t s in t h e sea s u r f a c e tempera ture (SST) estimation. Ch. 4 and ch. 5 of AVHRR occupy t h e ad jacent thermal in f ra red bands in t h e atmospheric window. The SST i s es t imated by a l inear function of those br ightness temperatures . For t h e purpose, two typical s t r u c t u r e s have been used, i. e., DVF (dcuble variable function): Y = cX4 bX5 + a SWF (split-window functicn) : = ( c b ) X ~ + b(X4-X.) + a Y = X 4 + g ( x 4 X ~ ) + d where Y i s t h e estimated SST, and X I and X 5 are t h e brightness tempera tures of ch. 4 and ch. 5, respectively. The s t r u c t u r e of SWF comes f rom t h e anlysis to t h e rad ia t ive t r a n s f e r equation. That is, t h e re lat ion between ( Y x , ) and ( X 4 X 5 ) can be approximated to be linear (Maclain 1981. McMillin and Crosby 1984) . Y i s meant t h e s e a t r u t h SST. There are o t h e r dis turbances in t h e SST estimation. Then DVF is introduced as a generalized s t r u c t u r e of SWF. Both DVF and SWF are linear functions, bu t they have d i f fe ren t degrees of freedom in the coefficients. DVF has of two f o r b and c. but SWF has of one f o r g only. The higher degree of freedom can be more flexible t o compensate collaborating e r r o r s totally. The coeff ic ients of SST estimation funct ions a r e usually calculated by applying the regression analysis t o match-up sets of Y. X 4 and X 5 observed direct ly o r indirectly. Table I is a l is t of SST estimation functions proposed by various authors . Both DVF and SWF exis t in the list , but i t is very interest ing that the var iat ions of the i r coeff ic ients remain v e r y small. That is. (1 ) ( c b ) remains near ly eqlual t o one, (2) b and g are r e s t r i c t e d in a narrow range, and (3) a and d are r e s t r i c t e d in a narrow range. Those s imilar i t ies have been understood as a supplementary proof of t h e e f fec t iveness of t h e split-window method (McMillin and Crosby 1 9 8 4 ) . 2 (XIEFFcms WE To m m m ANALYSIS Asaune that a set of mat&-ups IS = { ( Y , , x4 ,. xs d I i l l -NI i s given, where y , , x 4 , and x5 , are observed values of Y , X I and X 5 at a c e r t a i n point and time. i i s the identification number and N is the total number of the match-ups. For general var iables of V and W. descr ibe t h e covariance and t h e cor re la t ion coeff ic ient of them as SV w and RV W . respectively. But f o r t h e convenience, t h e descriptions will be abbreviated as follows. Sx4.x4 4 S . 4 . S X 5 . X S 4 s 5 5 , su Y 4 s w , s x 4 .x5 4 s4 5 . su. x 4 4 s u 4 , s u x 5 4 sus, R x 4 .x5 4 R 4 s . R y . x 4 4 Rv4 , R u . x 5 4 R u 5 The next formulas are obviious f rom t h e s ta t i s t ica l theory. 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引用次数: 0

摘要

在利用AVHRR资料的窗口法估算海表温度(SST)的过程中,回归分析中一般假设两种类型的海表温度(SST)。DVF: Y = (c-b)X4 + b(X4- x5) + a SWF: Y = X4 + g (X4 X ~) + d,其中Y、X4和X5为最测得的海表温度。这是第4和第5波段的亮度温度。DVF系数中的自由度为2,而SWF系数中的自由度为1。然而,在2008年的许多实证结果中,DVF具有与主权财富基金相似的系数。本文研究了该方法的相似之处,并证明了该方法来自于该方法的特定特性,该方法是由该方法提供的一组分窗。利用Mutsu Bay配对模型进行了模拟,验证了这一结论。分窗法被认为是一种很好的方法,它可以准确地估计大气温度,而不是海洋温度,这是估计海洋温度的最佳方法。AVHRR的第4和第5波段占据了大气窗口的近红外波段。海温是用这些亮度温度的线性函数来模拟的。t h e的目的,两个典型t r u c t u r e年代已经使用,即DVF (dcuble变量函数):Y = cX4 bX5 +一个SWF (split-window functicn): = (c b) X ~ + b (X4-X) + Y = X 4 + g (X 4 X ~) + d、我在哪里Y s t h e估计海温和X, X 5 t h e亮度温度的ch。4和ch。5,分别。SWF的s = r = r,而s = r = r则来自于对s = r方程的分析。也就是说,(Y x,)和(x 4 x 5)之间的关系可以近似为线性关系(Maclain 1981)。麦克米林和克罗斯比1984)。它的意思是说,它的意思是,它的意思是,它的意思是,它的意思是,它的意思是,它的意思是,它的意思是,它的意思是。在海表温度估计中不存在任何干扰。然后将DVF作为广义的广义广义函数引入到SWF中。DVF和SWF都是线性函数,但它们的系数有5个自由度。DVF有2个b和c,而SWF只有1个g。更高的自由度可以更灵活地补偿协作,或者完全补偿协作。海表温度估计函数的系数通常是通过对Y. X 4和X 5的直接或间接观测配对集进行回归分析来计算的。表1是各作者提出的海表温度估计函数的l和t。DVF和SWF都在列表中,但非常有趣的是,它们的变化仍然非常小。这是。(1) (c b)与1保持接近相等,(2)b和g在较窄的范围内与1相等,(3)a和d在较窄的范围内与1相等,(3)a和d在较窄的范围内与1相等。这些相似的方法被认为是对分窗法的有效性和有效性的补充证明(McMillin and Crosby 1994)。2 (1) m m m m n n n n n n n n n n n n n n n n n n n n n n n n n n n n其中,y、、x 4、x5为y、x I、x5在某一时刻的观测值,x I、x5在某一时刻的观测值。i是识别号,N是配对的总次数。对于一般变量V和w,将它们的协方差和相关系数分别描述为SV w和RV w。分别。但是为了方便起见,我们将这些描述简化如下。Sx4。x4 4 S。4 . 5。X 4 S 5 5, Y 4 S w, X 4, X 5 4 S 5。x 4 4 s, x 4 s, x 4 s, x 4 s, x 4 s。R y。x 4 4 Rv4, R u。下一个公式是很明显的,从这个公式可以看出这是一个理论。S45 = r4 5 E X E, Sv4 = r4 / X X T, (1)
本文章由计算机程序翻译,如有差异,请以英文原文为准。
On the characteristics of Coefficients in SST Estimation Functions by Split-Window Method
In t h e sea s u r f a c e temperature (SST) estimation by t h e window method f o r AVHRR da ta , two kinds of s t r u c t u r e are popularly assumed in t h e regression analysis. DVF: Y = (c-b)X4 + b(X4-X5) + a SWF: Y = X 4 + g ( x 4 X ~ ) + d where Y , X 4 and X 5 are t h e est imated SST. t h e br ightness tanmatures of ch. 4 and ch. 5 , respectively. The degree of freedom in the coeff ic ient of DVF is two, bu t t h a t of SWF is one. In many empirical resu l t s , however, DVF has similar coeff ic ients t o those in SWF. In th i s paper, t h e s imilar i ty of coeff ic ients i s investigated and showed t h a t i t comes from t h e specif ic charac te r i s t ics of t h e d a t a set provided by t h e split-windows. The assertion was confirmed by t h e simulation by using Mutsu Bay match-up d a t a set. 1 I " X 1 0 N The split-window method is known as an excellent algorithm f o r the correct ion of t h e atmospheric e f f e c t s in t h e sea s u r f a c e tempera ture (SST) estimation. Ch. 4 and ch. 5 of AVHRR occupy t h e ad jacent thermal in f ra red bands in t h e atmospheric window. The SST i s es t imated by a l inear function of those br ightness temperatures . For t h e purpose, two typical s t r u c t u r e s have been used, i. e., DVF (dcuble variable function): Y = cX4 bX5 + a SWF (split-window functicn) : = ( c b ) X ~ + b(X4-X.) + a Y = X 4 + g ( x 4 X ~ ) + d where Y i s t h e estimated SST, and X I and X 5 are t h e brightness tempera tures of ch. 4 and ch. 5, respectively. The s t r u c t u r e of SWF comes f rom t h e anlysis to t h e rad ia t ive t r a n s f e r equation. That is, t h e re lat ion between ( Y x , ) and ( X 4 X 5 ) can be approximated to be linear (Maclain 1981. McMillin and Crosby 1984) . Y i s meant t h e s e a t r u t h SST. There are o t h e r dis turbances in t h e SST estimation. Then DVF is introduced as a generalized s t r u c t u r e of SWF. Both DVF and SWF are linear functions, bu t they have d i f fe ren t degrees of freedom in the coefficients. DVF has of two f o r b and c. but SWF has of one f o r g only. The higher degree of freedom can be more flexible t o compensate collaborating e r r o r s totally. The coeff ic ients of SST estimation funct ions a r e usually calculated by applying the regression analysis t o match-up sets of Y. X 4 and X 5 observed direct ly o r indirectly. Table I is a l is t of SST estimation functions proposed by various authors . Both DVF and SWF exis t in the list , but i t is very interest ing that the var iat ions of the i r coeff ic ients remain v e r y small. That is. (1 ) ( c b ) remains near ly eqlual t o one, (2) b and g are r e s t r i c t e d in a narrow range, and (3) a and d are r e s t r i c t e d in a narrow range. Those s imilar i t ies have been understood as a supplementary proof of t h e e f fec t iveness of t h e split-window method (McMillin and Crosby 1 9 8 4 ) . 2 (XIEFFcms WE To m m m ANALYSIS Asaune that a set of mat&-ups IS = { ( Y , , x4 ,. xs d I i l l -NI i s given, where y , , x 4 , and x5 , are observed values of Y , X I and X 5 at a c e r t a i n point and time. i i s the identification number and N is the total number of the match-ups. For general var iables of V and W. descr ibe t h e covariance and t h e cor re la t ion coeff ic ient of them as SV w and RV W . respectively. But f o r t h e convenience, t h e descriptions will be abbreviated as follows. Sx4.x4 4 S . 4 . S X 5 . X S 4 s 5 5 , su Y 4 s w , s x 4 .x5 4 s4 5 . su. x 4 4 s u 4 , s u x 5 4 sus, R x 4 .x5 4 R 4 s . R y . x 4 4 Rv4 , R u . x 5 4 R u 5 The next formulas are obviious f rom t h e s ta t i s t ica l theory. S45 = R 4 5 E X E , Sv4 = R u 4 / X X T , ( 1 )
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