Observational studyaims at the approach to a dynamic system whose equation is undeterminable.

该方程组的解在有限时段上的采样值与给定序列重合。

The research tools are the vision-eikon-compare test 1 and test 2.

挑选受试者在同一时段先进行前测卷，再进行后测卷，测试完毕后再进行比较分析。

The syzygial tide is that the maximum amplitude period of semi-monthly tide added to the semi-diurnal and full-diurnal tides.

朔望潮即是半月潮度最大时段再迭加半日潮和全日潮。

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在一起,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。

Observational studyaims at the approach to a dynamic system whose equation is undeterminable.

该方程组的解在有限时段上的采样值与给定序列重合。

The research tools are the vision-eikon-compare test 1 and test 2.

挑选受试者在同一时段先进行前测卷，再进行后测卷，测试完毕后再进行比较分析。

The syzygial tide is that the maximum amplitude period of semi-monthly tide added to the semi-diurnal and full-diurnal tides.

朔望潮即是半月潮度最大时段再迭加半日潮和全日潮。

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在一起,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。

Observational studyaims at the approach to a dynamic system whose equation is undeterminable.

程组的解在有限时段上的采样值与给定序列重合。

The research tools are the vision-eikon-compare test 1 and test 2.

挑选受试者在同一时段先进行前测卷，再进行后测卷，测试完毕后再进行比较分析。

The syzygial tide is that the maximum amplitude period of semi-monthly tide added to the semi-diurnal and full-diurnal tides.

朔望潮即是半月潮度最大时段再迭加半日潮和全日潮。

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在一起,提出了用时随机函数观点去分析水文数据的多时段余协克立格模型。

Observational studyaims at the approach to a dynamic system whose equation is undeterminable.

该方程组的解在有限时段上的采样值与给定序列重合。

The research tools are the vision-eikon-compare test 1 and test 2.

挑选受试者在同一时段先进行前测卷，再进行后测卷，测试完毕后再进行比较分。

The syzygial tide is that the maximum amplitude period of semi-monthly tide added to the semi-diurnal and full-diurnal tides.

潮即是月潮度最大时段再日潮和全日潮。

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在一起,提出了用时空随机函数观点去分水文数据的多时段空间剩余协克立格模型。

Observational studyaims at the approach to a dynamic system whose equation is undeterminable.

该方程组的解在有限段上的采样值与给定序列重合。

The research tools are the vision-eikon-compare test 1 and test 2.

挑选受试者在同一段先进行前测卷，再进行后测卷，测试完毕后再进行比较分析。

The syzygial tide is that the maximum amplitude period of semi-monthly tide added to the semi-diurnal and full-diurnal tides.

朔望潮即潮度段再迭加日潮和全日潮。

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在一起,提出了用空随机函数观点去分析水文数据的多段空间剩余协克立格模型。

Observational studyaims at the approach to a dynamic system whose equation is undeterminable.

该方程组的解在有限段上的采样值与给定合。

The research tools are the vision-eikon-compare test 1 and test 2.

挑选受试者在同一段先进行前测卷，再进行后测卷，测试完毕后再进行比较分析。

The syzygial tide is that the maximum amplitude period of semi-monthly tide added to the semi-diurnal and full-diurnal tides.

朔望潮即是半月潮度最大段再迭加半日潮和全日潮。

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在一起,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。

Observational studyaims at the approach to a dynamic system whose equation is undeterminable.

该方程组的解在有限段上的采样值与给定序列重合。

The research tools are the vision-eikon-compare test 1 and test 2.

挑选受试者在段先进行前测卷，再进行后测卷，测试完毕后再进行比较分析。

The syzygial tide is that the maximum amplitude period of semi-monthly tide added to the semi-diurnal and full-diurnal tides.

朔望潮即是半月潮度最大段再迭加半日潮和全日潮。

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

本文将随水文学理论和质数学理论有合在起,提出了用空随函数观点去分析水文数据的多段空间剩余协克立格模型。

Observational studyaims at the approach to a dynamic system whose equation is undeterminable.

该方程组的解在有限时段上的采样值与给定序列重合。

The research tools are the vision-eikon-compare test 1 and test 2.

挑选受者在同一时段先进行前卷，再进行后卷，毕后再进行比较分析。

The syzygial tide is that the maximum amplitude period of semi-monthly tide added to the semi-diurnal and full-diurnal tides.

朔望潮即是半月潮度最大时段再迭加半日潮和全日潮。

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

本文水文学理论和地质数学理论有地结合在一起,提出了用时空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。

Observational studyaims at the approach to a dynamic system whose equation is undeterminable.

该方程组的解在有限时段上的采样值与给定序列重合。

The research tools are the vision-eikon-compare test 1 and test 2.

挑选受试者在同一时段先进行前测卷，再进行后测卷，测试完毕后再进行比较分析。

The syzygial tide is that the maximum amplitude period of semi-monthly tide added to the semi-diurnal and full-diurnal tides.

朔望潮即是半月潮度最大时段再迭加半日潮和全日潮。

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在一起,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。

Observational studyaims at the approach to a dynamic system whose equation is undeterminable.

该方程组有限时段上采样值与给定序列重合。

The research tools are the vision-eikon-compare test 1 and test 2.

挑选受试者同一时段先进行前测卷，再进行后测卷，测试完毕后再进行比较分析。

The syzygial tide is that the maximum amplitude period of semi-monthly tide added to the semi-diurnal and full-diurnal tides.

朔望潮即是半月潮度最大时段再迭加半日潮和全日潮。

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,提出了用时空随机函观点去分析水文多时段空间剩余协克立格模型。