applied hydrology rslab-ntu lab for remote sensing hydrology and spatial modeling 1 detection of...

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1 Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling Detection of Hydrological Changes – Nonparametric Approaches Professor Ke-Sheng Cheng Dept. of Bioenvironmental Systems Engineering National Taiwan University

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Page 1: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

1

Applied Hydrology

RSLAB-NTU

Lab for Remote Sensing Hydrology and Spatial Modeling

Detection of Hydrological Changes – Nonparametric Approaches

Professor Ke-Sheng ChengDept. of Bioenvironmental Systems Engineering

National Taiwan University

Page 2: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

2Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Parametric vs nonparametric

Parametric statisticsBody of statistical methods based on an

assumed model for the underlying population from which the data was sampled.

Inference is about some parameter (mean, variance, correlation) of the population•

If model is incorrect the inference may be misleading.

Example: Classical t-test assumes normal populations.

Page 3: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

3Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Nonparametric statisticsBody of statistical methods that relax the assum

ptions about the underlying population model.Typically statistics based on ranks or simple co

unts.Can be used for both ordinal and nominal data.

Page 4: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

4Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

MWP test for change point detection

Page 5: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

5Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Page 6: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

6Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Let us suppose the Xi are independent

Bernoulli random variables.

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Page 7: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

7Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Page 8: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

8Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

m

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Page 9: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

9Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Page 10: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

10Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Page 11: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

11Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Page 12: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

12Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Assessment on the performance of MWP test

In general, the time of change occurrence is detected at a time that occurs later than the real time of change occurrence. [The problem of late detection.]

Page 13: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

13Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Mann-Kendall test for trend detection

The Mann-Kendall trend test is derived from a rank correlation test for two groups of observations.

In the Mann-Kendall trend test, the correlation between the rank order of the observed values and their order in time is considered.

The null hypothesis for the Mann-Kendall test is that the data are independent and randomly ordered, i.e. there is no trend or serial correlation structure among the observations.

Page 14: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

14Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

However, in many real situations the observed data are autocorrelated. The autocorrelation in observed data will result in misinterpretation of trend tests results.

Positive serial correlation among the observations would increase the chance of significant answer, even in the absence of a trend.

Page 15: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

15Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

The original Mann-Kendall trend test

Page 16: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

16Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Under the null hypothesis that X and Y are independent and randomly ordered, the statistic S tends to normality for large n, with mean and variance given by:

Page 17: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

17Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

If the values in Y are replaced with the time order of the time series X, i.e. 1,2,...,n, the test can be used as a trend test. In this case, the statistic S reduces to that given in Eq. (5):

Page 18: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

18Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Kendall (1955) gives a proof of the asymptotic normality of the statistic S. The significance of trends is tested by comparing the standardized test statistic Z = with the standard normal variate at the desired significance level.

)var(SS

Page 19: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

19Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Autocorrelated data series

If X is normally distributed with mean and variance 2, then (xj – xi) will also be normally di

stributed with mean zero and variance 22.

Page 20: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

20Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

It can be shown that for autocorrelated data series var(S) is the same as that of independent series, i.e.,

Page 21: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

21Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

The assumption of normally distributed X was used to derive the above results, but in fact the test is nonparametric and does not depend on the distribution of X.

Page 22: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

22Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

The effect of autocorrelation on the Mann-Kendall trend test

Fig. 1 shows two time series X and Y each of length n = 100 observations.

Visual inspection of the two time series would not indicate a large difference in the apparent trends for the two series.

In fact, series X is stationary white noise, while series Y is generated as an AR(1) series with = 0.4 using series X as the input noise.

Both series are stationary without trend.

Page 23: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

23Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Page 24: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

24Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Page 25: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

25Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Page 26: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

26Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Page 27: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

27Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Autocorrelation between the ranks of the observations

Page 28: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

28Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Page 29: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

29Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Approximate formula for calculating V(S)

Page 30: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

30Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Page 31: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

31Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Page 32: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

32Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Page 33: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

33Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU

Page 34: Applied Hydrology RSLAB-NTU Lab for Remote Sensing Hydrology and Spatial Modeling 1 Detection of Hydrological Changes – Nonparametric Approaches Professor

34Lab for Remote Sensing Hydrology and Spatial ModelingRSLAB-NTU