Dynamic Panel Modeling of Climate Change

P. Phillips
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引用次数: 4

Abstract

We discuss some conceptual and practical issues that arise from the presence of global energy balance effects on station level adjustment mechanisms in dynamic panel regressions with climate data. The paper provides asymptotic analyses, observational data computations, and Monte Carlo simulations to assess the use of various estimation methodologies, including standard dynamic panel regression and cointegration techniques that have been used in earlier research. The findings reveal massive bias in system GMM estimation of the dynamic panel regression parameters, which arise from fixed effect heterogeneity across individual station level observations. Difference GMM and Within Group (WG) estimation have little bias and WG estimation is recommended for practical implementation of dynamic panel regression with highly disaggregated climate data. Intriguingly, from an econometric perspective and importantly for global policy analysis, it is shown that in this model despite the substantial differences between the estimates of the regression model parameters, estimates of global transient climate sensitivity (of temperature to a doubling of atmospheric CO2) are robust to the estimation method employed and to the specific nature of the trending mechanism in global temperature, radiation, and CO2.
气候变化动态面板模拟
本文讨论了气候资料动态面板回归中全球能量平衡对站位平差机制的影响所引起的一些概念和实际问题。本文提供了渐近分析、观测数据计算和蒙特卡罗模拟,以评估各种估计方法的使用,包括早期研究中使用的标准动态面板回归和协整技术。研究结果表明,动态面板回归参数的系统GMM估计存在巨大偏差,这是由单个站水平观测的固定效应异质性引起的。差分GMM和组内(WG)估计偏差较小,在实际实现高度分解气候数据的动态面板回归时,推荐使用WG估计。有趣的是,从计量经济学的角度和重要的全球政策分析来看,在该模型中,尽管回归模型参数的估计值之间存在实质性差异,但全球瞬态气候敏感性(温度对大气CO2增加一倍)的估计值对于所采用的估计值方法以及全球温度、辐射和CO2趋势机制的具体性质是稳健的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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