[1] Hydroclimatological time series often exhibit trends. While trend magnitude can be determined with little ambiguity, the corresponding statistical significance, sometimes cited to bolster scientific and political argument, is less certain because significance depends critically on the null hypothesis which in turn reflects subjective notions about what one expects to see. We consider statistical trend tests of hydroclimatological data in the presence of long-term persistence (LTP). Monte Carlo experiments employing FARIMA models indicate that trend tests which fail to consider LTP greatly overstate the statistical significance of observed trends when LTP is present. A new test is presented that avoids this problem. From a practical stan...
Hydrological time series increasingly exhibit non-stationarity, e.g., variables such as precipitatio...
<p>The long-term persistence (LTP), else known in hydrological science as the Hurst phenomenon, is a...
The widely-used hydrological procedures for calculating events with T-year return periods from data ...
Today, hydrologic research and modeling depends largely on climatological inputs, whose physical and...
Today, hydrologic research and modeling depends largely on climatological inputs, whose physical and...
Although persistence in natural data is generally admitted, its effect on the significance of variou...
The Mann–Kendall (MK) test was widely used to detect significant trends in hydrologic and climate ti...
Theoretical arguments and climate projections suggest that extreme precipitations are expected to in...
The detection and attribution of long-term patterns in hydrological time series have been important ...
The detection and attribution of long-term patterns in hydrological time series have been important ...
Hydroclimatic processes such as precipitation, temperature, wind speed and dew point are usually con...
In the last decades the growing concerns about the existence of global climatic changes push many r...
The detection and attribution of long-term patterns in hydrological time series have been important ...
[1] Trends in hydrologic sequences may be assessed in various ways. The coefficient of regression of...
In the last decades the growing concerns about the existence of global climatic changes push many re...
Hydrological time series increasingly exhibit non-stationarity, e.g., variables such as precipitatio...
<p>The long-term persistence (LTP), else known in hydrological science as the Hurst phenomenon, is a...
The widely-used hydrological procedures for calculating events with T-year return periods from data ...
Today, hydrologic research and modeling depends largely on climatological inputs, whose physical and...
Today, hydrologic research and modeling depends largely on climatological inputs, whose physical and...
Although persistence in natural data is generally admitted, its effect on the significance of variou...
The Mann–Kendall (MK) test was widely used to detect significant trends in hydrologic and climate ti...
Theoretical arguments and climate projections suggest that extreme precipitations are expected to in...
The detection and attribution of long-term patterns in hydrological time series have been important ...
The detection and attribution of long-term patterns in hydrological time series have been important ...
Hydroclimatic processes such as precipitation, temperature, wind speed and dew point are usually con...
In the last decades the growing concerns about the existence of global climatic changes push many r...
The detection and attribution of long-term patterns in hydrological time series have been important ...
[1] Trends in hydrologic sequences may be assessed in various ways. The coefficient of regression of...
In the last decades the growing concerns about the existence of global climatic changes push many re...
Hydrological time series increasingly exhibit non-stationarity, e.g., variables such as precipitatio...
<p>The long-term persistence (LTP), else known in hydrological science as the Hurst phenomenon, is a...
The widely-used hydrological procedures for calculating events with T-year return periods from data ...