Description Usage Arguments Details Value Author(s) References Examples

This function calculates the significance of the departure from the mean for a given set of key event years and lagged years.

1 |

`x` |
a chronology |

`key` |
a vector specifying the key event years for the superposed epoch |

`lag` |
an integral value defining the number of lagged years |

`resample` |
an integral value specifying the number of bootstrap sample for calculation of confidence intervals |

Superposed epoch analysis (SEA) is used to test the significance of a mean
tree growth response to certain events (such as droughts). Departures
from the mean RWI values for the specified years prior to
each event year, the event year, and the specified years immediately
after each event are averaged to a superposed epoch. To determine if
RWI for these years was significantly different from
randomly selected sets of

other years, bootstrap
resampling is used to randomly select sets of `lag`+1

years
from the data set and to estimate significances for the departures
from the mean RWI.
`lag`+1

SEA computation is based on scaled RWI values, and 95%-confidence intervals are computed for the scaled values for each year in the superposed epoch.

A `data.frame`

with

`lag` |
the lagged years, |

`se` |
the superposed epoch, i.e. the scaled mean RWI for the event years, |

`se.unscaled` |
the unscaled superposed epoch, i.e. the mean RWI for the event years, |

`p` |
significance of the departure from the chrono’s mean RWI, |

`ci.95.lower` |
lower 95% confidence band, |

`ci.95.upper` |
upper 95% confidence band, |

`ci.99.lower` |
lower 99% confidence band, |

`ci.99.upper` |
upper 99% confidence band. |

Christian Zang. Patched and improved by Mikko Korpela.

Lough, J. M. and Fritts, H. C. (1987) An assessment of the possible
effects of volcanic eruptions on North American climate using
tree-ring data, 1602 to 1900 AD. *Climatic Change*,
**10**(3), 219–239.

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dplR documentation built on Nov. 5, 2018, 5:06 p.m.

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