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。

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

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在一起,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。

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

该方程组的解在有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.

朔望潮即是半月潮度最大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.

本将随机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数据的多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。

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在一起,提出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.

挑者在同时段先进行前测卷，再进行后测卷，测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,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。

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前卷，再进卷，试完毕再进比较分析。

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.

本将随机水论和地质数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.

挑选受试者在同一先进行前测卷，再进行后测卷，测试完毕后再进行比较。

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文数据的多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行前测卷，行测卷，测试完毕行比较分析。

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

朔望即是半月度最大时段迭加半和全。

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格模型。

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

该方程组的解在有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.

本将随机学理论和地质学理论有机地结合在一起,提出了用空随机函观点去分析据的多段空间剩余协克立格模型。