Show simple item record

dc.contributor.advisorSørbye, Sigrunn Holbek
dc.contributor.authorMyrvoll-Nilsen, Eirik
dc.date.accessioned2020-04-29T06:53:37Z
dc.date.available2020-04-29T06:53:37Z
dc.date.issued2020-05-22
dc.description.abstractTemperature fluctuations can be described by a persistent correlation structure known as long-range dependence (LRD). This is a phenomenon which implies that the autocorrelation function follows a power-law decay and that observations may still be significantly correlated even if the temporal or spatial distance between them is large. Moreover, temperature is known to be influenced by radiative forcing, or how much of the solar radiation is absorbed by the earth. This is affected by factors such as solar variation and emission of climate gases. The topic of this thesis is to develop efficient statistical methodology to obtain Bayesian inference for global and local climatic time series data. This is achieved using the general hierarchical modeling framework of latent Gaussian models. Bayesian analysis can be performed efficiently using the methodology of integrated nested Laplace approximation (INLA), utilising the sparse structure of the inverse covariance matrix of the latent Gaussian field. Obtaining inference for LRD processes using INLA is inefficient on account of their dense inverse covariance matrix. Paper I demonstrates how stationary Gaussian LRD processes with memory governed by a single-parameter can be approximated with great accuracy using a mixture of four first-order autoregressive processes. This approximation ensures that the LRD model retains conditional independence and that inference can be obtained in linear time and memory. Paper II details how this methodology can be used to design a Bayesian model for global mean surface temperature (GMST) that reflects climate dynamics by incorporating radiative forcing data. This model is available as the R-package INLA.climate and is used to estimate the transient climate response and to predict temperature response to future forcing scenarios. Paper III uses the GMST model to estimate equilibrium climate sensitivity, and paper IV applies the same methodology to gridded local time series.en_US
dc.description.doctoraltypeph.d.en_US
dc.description.popularabstractSince the industrial revolution the temperature on Earth has increased substantially due to increased radiative forcing. This is defined as the imbalance between incoming and outgoing radiation in the climatic system and is affected by factors such as emission of climate gases. Moreover, climatic time series are known to exhibit long memory, which implies that even distant variables can be correlated. This can make obtaining statistical inference very computationally difficult. We overcome this by approximating long memory processes as a mixture of short memory processes. This was found to be remarkably accurate, even when using just four short memory processes. This grants us a major reduction in computational cost and allows us to incorporate this into a general modeling framework which can be used to estimate how susceptible the climate system is to increased CO2-emission, perform temperature prediction given possible scenarios for future forcing and analyse local time series data.en_US
dc.description.sponsorshipFinansiering: UiT Rekrutteringsstillingen_US
dc.identifier.isbn978-82-8236-397-6
dc.identifier.urihttps://hdl.handle.net/10037/18148
dc.language.isoengen_US
dc.publisherUiT Norges arktiske universiteten_US
dc.publisherUiT The Arctic University of Norwayen_US
dc.relation.haspartPaper I: Sørbye, S.H., Myrvoll-Nilsen, E. & Rue, H. (2019). An approximate fractional Gaussian noise model with O(n) computational cost. <i>Statistics and Computing, 29</i>, 821–833. Also available at <a href=https://doi.org/10.1007/s11222-018-9843-1>https://doi.org/10.1007/s11222-018-9843-1. </a> <p> <p>Paper II: Myrvoll-Nilsen, E., Sørbye, S.H., Fredriksen, H.-B., Rue, H. & Rypdal, M. (2020). Statistical estimation of global surface temperature response to forcing under the assumption of temporal scaling. (Submitted manuscript). Final version published in <i>Earth System Dynamics, 11</i>, 329-345, is available at <a href=https://doi.org/10.5194/esd-11-329-2020>https://doi.org/10.5194/esd-11-329-2020. </a> <p> <p>Paper III: Rypdal, M., Fredriksen, H.-B., Myrvoll-Nilsen, E., Rypdal, K. & Sørbye, S.H. (2018). Emergent Scale Invariance and Climate Sensitivity. <i>Climate, 6</i>(4), 93. Also available in Munin at <a href=https://hdl.handle.net/10037/15254>https://hdl.handle.net/10037/15254. </a><p> <p>Paper IV: Myrvoll-Nilsen, E., Fredriksen, H.-B., Sørbye, S.H. & Rypdal, M. (2019). Warming trends and long-range dependent climate variability since year 1900: a Bayesian approach. <i>Frontiers in Earth Science, 7</i>:214. Also available in Munin at <a href=https://hdl.handle.net/10037/17054>https://hdl.handle.net/10037/17054. </a>en_US
dc.rights.accessRightsopenAccessen_US
dc.rights.holderCopyright 2020 The Author(s)
dc.subject.courseIDDOKTOR-004
dc.subjectVDP::Mathematics and natural science: 400::Mathematics: 410::Statistics: 412en_US
dc.subjectVDP::Matematikk og Naturvitenskap: 400::Matematikk: 410::Statistikk: 412en_US
dc.titleEfficient Bayesian analysis of long memory processes applied to climateen_US
dc.typeDoctoral thesisen_US
dc.typeDoktorgradsavhandlingen_US


File(s) in this item

Thumbnail
Thumbnail

This item appears in the following collection(s)

Show simple item record