This paper defines the news impact curve — a graphical and analytical device for showing how a volatility model translates the latest return shock into next period's conditional variance — and uses it to compare symmetric and asymmetric ARCH models. Motivated by the leverage effect (bad news raises volatility more than good news of the same size), Engle and Ng introduce new diagnostic tests for asymmetry, propose a partially nonparametric (PNP) model that lets the data trace out the news-volatility relation, and estimate the competing models on daily Japanese (TOPIX) stock returns. They conclude that the Glosten-Jagannathan-Runkle (GJR) model is the best parametric specification, while EGARCH captures the asymmetry but implies an excessively variable conditional variance.
"This paper defines the news impact curve which measures how new information is incorporated into volatility estimates."
"Our results suggest that the model by Glosten, Jagannathan, and Runkle is the best parametric model. The EGARCH also can capture most of the asymmetry; however, there is evidence that the variability of the conditional variance implied by the EGARCH is too high."
The news impact curve is one of those small conceptual inventions that outlasts its paper: it turns an abstract comparison of volatility recursions into a single picture — how does this model react to this shock? — and immediately makes the leverage asymmetry visible as a curve that is not symmetric about zero. The sign- and size-bias tests are the practical companion: they let you diagnose that a symmetric GARCH is missing something without committing to which asymmetric model to use. For the wiki this is the diagnostic backbone of the GARCH page's asymmetric-model material (EGARCH, GJR, power-GARCH), and it pairs naturally with the volatility-forecast-evaluation and news-driven stochastic-volatility threads. The verdict favoring GJR over EGARCH has aged well, though the choice is data-dependent and later work finds the ranking sensitive to the return series and sample.