Skip to main content

Official Journal of the Asia Oceania Geosciences Society (AOGS)

Table 1 Trend types of non-stationary GEV model

From: Extreme precipitation trends in Northeast China based on a non-stationary generalized extreme value model

Trend types

Parameter forms

\(\mu\) linear trend, \(\sigma\) no trend (AL)

\(\mu \left(t\right)={\mu }_{0}+{\mu }_{1}t, \sigma \left(t\right)={\sigma }_{0}\)

\(\mu\) parabolic trend, \(\sigma\) no trend (AP)

\(\mu \left(t\right)={\mu }_{0}+{\mu }_{1}t+{\mu }_{2}{t}^{2}, \sigma \left(t\right)={\sigma }_{0}\)

\(\mu\) no trend, \(\sigma\) linear trend (BL)

\(\mu \left(t\right)={\mu }_{0}, \sigma \left(t\right)={\sigma }_{0}+{\sigma }_{1}t\)

\(\mu\) no trend, \(\sigma\) parabolic trend (BP)

\(\mu \left(t\right)={\mu }_{0}, \sigma \left(t\right)={\sigma }_{0}+{\sigma }_{1}t+{\sigma }_{2}{t}^{2}\)

\(\mu\) linear trend, \(\sigma\) linear trend (DL)

\(\mu \left(t\right)={\mu }_{0}+{\mu }_{1}t, \sigma \left(t\right)={\sigma }_{0}+{\sigma }_{1}t\)