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NEW ASYMPTOTICS APPLIED TO FUNCTIONAL COEFFICIENT REGRESSION AND CLIMATE SENSITIVITY ANALYSIS

Published online by Cambridge University Press:  11 February 2026

Qiying Wang*
Affiliation:
The University of Sydney
Peter C. B. Phillips
Affiliation:
Yale University, University of Auckland, and Singapore Management University
Ying Wang
Affiliation:
Renmin University of China
*
Address correspondence to Qiying Wang, School of Mathematics and Statistics, The University of Sydney, Australia, e-mail: qiying.wang@sydney.edu.au.
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Abstract

A general asymptotic theory is established for sample cross moments of nonstationary time series, allowing for long-range dependence and local unit roots. The theory provides a substantial extension of earlier results on nonparametric regression that include near-cointegrated nonparametric regression as well as spurious nonparametric regression. Many new models are covered by the limit theory, among which are functional coefficient regressions in which both regressors and the functional covariate are nonstationary. Simulations show finite sample performance matching well with the asymptotic theory and having broad relevance to applications, while revealing how dual nonstationarity in regressors and covariates raises sensitivity to bandwidth choice and the impact of dimensionality in nonparametric regression. An empirical example is provided involving climate data regression to assess Earth’s climate sensitivity to CO$_2$, where nonstationarity is a prominent feature of both the regressors and covariates in the model. To our knowledge, this application is the first nonparametric empirical analysis to assess potential nonlinear impacts of CO$_2$ on Earth’s climate while allowing for nonstationarity in both the regressors and covariates.

Information

Type
ARTICLES
Copyright
© The Author(s), 2026. Published by Cambridge University Press
Figure 0

Table 1 Finite sample mean bias and standard error (in square brackets) of the local level estimator $\hat {\beta }_n(x)$ at point $x=0$ for model M1 with $h=0.5n^{\gamma }$

Figure 1

Table 2 Finite sample mean bias and standard error (in square brackets) of the local linear estimator $\hat {\beta }_L(x)$ at point $x=0$ for model M1 with $h=0.5n^{\gamma }$

Figure 2

Table 3 Finite sample mean bias and standard error (in square brackets) of the local level estimator at point $x=0$ for model M2 with bandwidth $h=1.5n^{-3/10}$

Figure 3

Table 4 Finite sample mean bias and standard error (in square brackets) of the local linear estimator at point $x=0$ for model M2 with bandwidth $h=2n^{-3/10}$

Figure 4

Figure 1 A representative demonstration of the curve estimates with $n=400$, $h=C_h n^{-3/10}$, $d=0,$ and $(\theta ,\lambda _1,\lambda _2)=(0,0,0)$.

Figure 5

Figure 2 A representative demonstration of the empirical densities of the self-normalized quantities given in Theorems 4.1–4.3 (equations (4.4), (4.9), and (4.13)) with $h=0.5n^{-3/10}$, $d=0,$ and $(\theta ,\lambda _1,\lambda _2)=(0,0,0)$.

Figure 6

Table 5 Finite sample size and local power of bootstrap procedure in model M2 with $d=0$

Figure 7

Table 6 Finite sample size and local power performance in model M2 with $d=0.4$ and $(\theta ,\lambda _1,\lambda _2)=(0,0,0)$

Figure 8

Figure 3 Time-series plot of station-averaged temperature ($\overline {T}_t$, $^{\circ }$Celsius; blue solid), downward surface radiation ($\bar {R}_t$, Watts per $m^2$; red dashed), and logarithms of CO$_2$ (Pg: metric gigatons; black dotted with circle markers) ranging from 1964 to 2005.

Figure 9

Figure 4 Estimated functional coefficients of model (6.1).

Figure 10

Figure 5 Estimated functional coefficient $\beta _0(\bar {R}_t)$ of model (6.2).