The concept of uniform convergence was proposed for the thorough research on the analyticity of the functions defined as limits.

要一致收敛概念是为深入研究极限函数的分析性质而提出的。

A multi-period spatial residual Cokriging model combining Stochastic Hydrology with Geomathematics,was used to analysis hydrology data with spatial and temporal random function.

本文将随机水文学理论和地质数学理论有机地结合一起,提出了用时空随机函数观点去分析水文数据的多时段空间剩余协克立格模型。

The concept of uniform convergence was proposed for the thorough research on the analyticity of the functions defined as limits.

摘要一致收敛概念是为深入限函数的分析性质而提出的。

A multi-period spatial residual Cokriging model combining Stochastic Hydrology with Geomathematics,was used to analysis hydrology data with spatial and temporal random function.

本文将随机水文学理论和地质数学理论有机地结合一起,提出了用时空随机函数观点去分析水文数据的多时段空间剩余协克立格模。

The concept of uniform convergence was proposed for the thorough research on the analyticity of the functions defined as limits.

摘要一致收敛概念是为深入研究极限函的分析性质而提出的。

A multi-period spatial residual Cokriging model combining Stochastic Hydrology with Geomathematics,was used to analysis hydrology data with spatial and temporal random function.

本文将随机水文学地质学有机地结合一起,提出了用时空随机函去分析水文据的多时段空间剩余协克立格模型。

The concept of uniform convergence was proposed for the thorough research on the analyticity of the functions defined as limits.

摘要一致收敛概念是为深入研究极限分析性质而提出。

A multi-period spatial residual Cokriging model combining Stochastic Hydrology with Geomathematics,was used to analysis hydrology data with spatial and temporal random function.

本文将随机水文学理论和地质学理论有机地结合一起,提出了用时空随机观点去分析水文据多时段空间剩余协模型。

The concept of uniform convergence was proposed for the thorough research on the analyticity of the functions defined as limits.

摘要致收敛概念是为深入研究极限函数的分析性质而出的。

A multi-period spatial residual Cokriging model combining Stochastic Hydrology with Geomathematics,was used to analysis hydrology data with spatial and temporal random function.

本文将随机水文学理论和质数学理论有机,出了用时空随机函数观点去分析水文数据的多时段空间剩余协克立格模型。

The concept of uniform convergence was proposed for the thorough research on the analyticity of the functions defined as limits.

摘要一致收敛为深入研究极限函数的分析质而提出的。

A multi-period spatial residual Cokriging model combining Stochastic Hydrology with Geomathematics,was used to analysis hydrology data with spatial and temporal random function.

本文将随机水文学理论和地质数学理论有机地结合一起,提出了用时空随机函数观点去分析水文数据的多时段空间剩余协克立格模型。

The concept of uniform convergence was proposed for the thorough research on the analyticity of the functions defined as limits.

摘要一致收敛概念是为深入研究极限函数的分析性质而提出的。

A multi-period spatial residual Cokriging model combining Stochastic Hydrology with Geomathematics,was used to analysis hydrology data with spatial and temporal random function.

本文将随机水文和地质数有机地结合一起,提出了随机函数观点去分析水文数据的多段间剩余协克立格模型。

The concept of uniform convergence was proposed for the thorough research on the analyticity of the functions defined as limits.

摘要一致收敛概念是为深入研究极限函数分析性质而提。

A multi-period spatial residual Cokriging model combining Stochastic Hydrology with Geomathematics,was used to analysis hydrology data with spatial and temporal random function.

文将随机水文学理论和地质数学理论有机地结合一起,提了用空随机函数观点去分析水文数据段空间剩余协克立格模型。

The concept of uniform convergence was proposed for the thorough research on the analyticity of the functions defined as limits.

摘要一致收敛概念是为深入研究极限函数的析性质而提出的。

A multi-period spatial residual Cokriging model combining Stochastic Hydrology with Geomathematics,was used to analysis hydrology data with spatial and temporal random function.

本文将随机水文学理论和地质数学理论有机地结合一起,提出了用时空随机函数观点去析水文数据的多时段空间剩余协克立格模型。