Based on the correlation principle, an algorithm to decomposite the damped free vibration signals of a two degrees of freedom system with close natural frequencies is put forward.

摘要一频率成分自由衰振动响应信号相关性原理，提出了一种频率密集成分两耦合振子自由衰振动响应信号解耦算法。

This homotopic method is an approximate analysis method, which can be more used for analyzing other behavior of the sea surface temperature anomaly of the atmosphere-ocean oscillator model.

本同伦方法是近似解析方法，它能进一步分析海-气振子海表温度异他性态。

Based on the correlation principle, an algorithm to decomposite the damped free vibration signals of a two degrees of freedom system with close natural frequencies is put forward.

摘要基于单一频率成的自由衰振动响应信号的相关性原理，提出了一种频率密集成的两耦合振子自由衰振动响应信号的解耦算法。

This homotopic method is an approximate analysis method, which can be more used for analyzing other behavior of the sea surface temperature anomaly of the atmosphere-ocean oscillator model.

本同伦方法是近似的的解析方法，它能进一步析海-气振子的海表温度异常的其他性态。

Based on the correlation principle, an algorithm to decomposite the damped free vibration signals of a two degrees of freedom system with close natural frequencies is put forward.

摘要基于单一频率成分的衰振信号的相关性原理，提出了一种频率密集成分的两耦合振衰振信号的解耦算法。

This homotopic method is an approximate analysis method, which can be more used for analyzing other behavior of the sea surface temperature anomaly of the atmosphere-ocean oscillator model.

本同伦方法是近似的的解析方法，它能进一步分析海-气振的海表温度异常的其他性态。

Based on the correlation principle, an algorithm to decomposite the damped free vibration signals of a two degrees of freedom system with close natural frequencies is put forward.

摘要基于单一频率成分的自由衰振动响应信号的相关性原理，提出了一种频率密集成分的两耦合振子自由衰振动响应信号的解耦算法。

This homotopic method is an approximate analysis method, which can be more used for analyzing other behavior of the sea surface temperature anomaly of the atmosphere-ocean oscillator model.

本同伦方法是近似的的解析方法，它能进一步分析海-气振子的海表温度异常的其他性态。

Based on the correlation principle, an algorithm to decomposite the damped free vibration signals of a two degrees of freedom system with close natural frequencies is put forward.

摘要基于单一频率成分的自动响应信号的相关性原理，提出了一种频率密集成分的两耦合子自动响应信号的解耦算法。

This homotopic method is an approximate analysis method, which can be more used for analyzing other behavior of the sea surface temperature anomaly of the atmosphere-ocean oscillator model.

本同伦方法是近似的的解析方法，它能进一步分析-子的表温度异常的其他性态。

Based on the correlation principle, an algorithm to decomposite the damped free vibration signals of a two degrees of freedom system with close natural frequencies is put forward.

摘要基于单一频率成分自由衰振动响应相关性原理，提出了一种频率密集成分两耦合振子自由衰振动响应解耦算法。

This homotopic method is an approximate analysis method, which can be more used for analyzing other behavior of the sea surface temperature anomaly of the atmosphere-ocean oscillator model.

本同伦方法是近似解析方法，一步分析海-气振子海表温度异常其他性态。

Based on the correlation principle, an algorithm to decomposite the damped free vibration signals of a two degrees of freedom system with close natural frequencies is put forward.

摘要基于单一成分的自由衰振动响应信号的相关性原理，提出了一种集成分的两耦合振子自由衰振动响应信号的解耦算法。

This homotopic method is an approximate analysis method, which can be more used for analyzing other behavior of the sea surface temperature anomaly of the atmosphere-ocean oscillator model.

本法是近似的的解析法，它能进一步分析海-气振子的海表温度异常的其他性态。

Based on the correlation principle, an algorithm to decomposite the damped free vibration signals of a two degrees of freedom system with close natural frequencies is put forward.

摘要基于单一频率成分自由衰动响应相关性原理，提出了一种频率密集成分两子自由衰动响应解算法。

This homotopic method is an approximate analysis method, which can be more used for analyzing other behavior of the sea surface temperature anomaly of the atmosphere-ocean oscillator model.

本同伦方法是近似解析方法，它能进一步分析海-气子海表温度异常其他性态。

Based on the correlation principle, an algorithm to decomposite the damped free vibration signals of a two degrees of freedom system with close natural frequencies is put forward.

摘要基于单一频率成分自由衰振动响应信号性原理，提出了一种频率密集成分两耦合振子自由衰振动响应信号解耦算法。

This homotopic method is an approximate analysis method, which can be more used for analyzing other behavior of the sea surface temperature anomaly of the atmosphere-ocean oscillator model.

本同伦法是近似解析法，能进一步分析海-气振子海表温度异常其他性态。