Response Functions for Arbitrary Weight Functions and Data Distributions. Part I: Framework for Interpreting the Response FunctionSource: Monthly Weather Review:;2005:;volume( 133 ):;issue: 008::page 2117DOI: 10.1175/MWR2961.1Publisher: American Meteorological Society
Abstract: The response function is a commonly used measure of analysis scheme properties. Its use in the interpretation of analyses of real-valued data, however, is unnecessarily complicated by the structure of the standard form of the Fourier transform. Specifically, interpretation using this form of the Fourier transform requires knowledge of the relationship between Fourier transform values that are symmetric about the origin. Here, these relationships are used to simplify the application of the response function to the interpretation of analysis scheme properties. In doing so, Fourier transforms are used because they can be applied to studying effects that both data sampling and weight functions have upon analyses. A complication arises, however, in the treatment of constant and sinusoidal input since they do not have Fourier transforms in the traditional sense. To handle these highly useful forms, distribution theory is used to generalize Fourier transform theory. This extension enables Fourier transform theory to handle both functions that have Fourier transforms in the traditional sense and functions that can be represented using Fourier series. The key step in simplifying the use of the response function is the expression of the inverse Fourier transform in a magnitude and phase form, which involves folding the integration domain onto itself so that integration is performed over only half of the domain. Once this is accomplished, interpretation of the response function is in terms of amplitude and phase modulations, which indicate how amplitudes and phases of input waves are affected by an analysis scheme. This interpretation is quite elegant since its formulation in terms of properties of input waves results in a one-to-one input-to-output wave interpretation of analysis scheme effects.
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contributor author | Askelson, Mark A. | |
contributor author | Straka, Jerry M. | |
date accessioned | 2017-06-09T17:27:02Z | |
date available | 2017-06-09T17:27:02Z | |
date copyright | 2005/08/01 | |
date issued | 2005 | |
identifier issn | 0027-0644 | |
identifier other | ams-85508.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4228963 | |
description abstract | The response function is a commonly used measure of analysis scheme properties. Its use in the interpretation of analyses of real-valued data, however, is unnecessarily complicated by the structure of the standard form of the Fourier transform. Specifically, interpretation using this form of the Fourier transform requires knowledge of the relationship between Fourier transform values that are symmetric about the origin. Here, these relationships are used to simplify the application of the response function to the interpretation of analysis scheme properties. In doing so, Fourier transforms are used because they can be applied to studying effects that both data sampling and weight functions have upon analyses. A complication arises, however, in the treatment of constant and sinusoidal input since they do not have Fourier transforms in the traditional sense. To handle these highly useful forms, distribution theory is used to generalize Fourier transform theory. This extension enables Fourier transform theory to handle both functions that have Fourier transforms in the traditional sense and functions that can be represented using Fourier series. The key step in simplifying the use of the response function is the expression of the inverse Fourier transform in a magnitude and phase form, which involves folding the integration domain onto itself so that integration is performed over only half of the domain. Once this is accomplished, interpretation of the response function is in terms of amplitude and phase modulations, which indicate how amplitudes and phases of input waves are affected by an analysis scheme. This interpretation is quite elegant since its formulation in terms of properties of input waves results in a one-to-one input-to-output wave interpretation of analysis scheme effects. | |
publisher | American Meteorological Society | |
title | Response Functions for Arbitrary Weight Functions and Data Distributions. Part I: Framework for Interpreting the Response Function | |
type | Journal Paper | |
journal volume | 133 | |
journal issue | 8 | |
journal title | Monthly Weather Review | |
identifier doi | 10.1175/MWR2961.1 | |
journal fristpage | 2117 | |
journal lastpage | 2131 | |
tree | Monthly Weather Review:;2005:;volume( 133 ):;issue: 008 | |
contenttype | Fulltext |