Analysis: Difference between revisions

From Glossary of Meteorology
imported>Perlwikibot
No edit summary
m (Rewrite with Template:Term and clean up)
 
(One intermediate revision by the same user not shown)
Line 1: Line 1:
 
{{Term
 
|Display title=analysis
{{TermHeader}}
|Definitions={{Definition
{{TermSearch}}
|Num=1
 
|Meaning=#In [[synoptic meteorology]], a detailed study of the state of the [[atmosphere]] based on  observations, usually including a separation of the entity into its component patterns and involving  the drawing of families of [[isopleths]] for various elements.
<div class="termentry">
|Explanation=Thus, the analysis of [[synoptic]] charts may consist, for example, of the drawing and the interpretation  of the patterns of [[wind]], [[pressure]], pressure change, [[temperature]], [[humidity]], [[clouds]],  and [[hydrometeors]], all based on observations taken or [[forecast]] simultaneously.<br/>  
  <div class="term">
#A procedure to project the state of the [[atmosphere]] (or any system) as known from a finite  set of imperfect, irregularly distributed observations onto a regular [[grid]] or to represent the atmospheric  state by the [[amplitude]] of [[standard]] mathematical functions.<br/> The grid and/or functional expansion allows for subsequent forecasts by [[numerical integration]]  or for easy diagnostic study. An analysis may be looked upon as a space&ndash;time [[interpolation]] system.  Essential ingredients of analysis are a [[background field]], usually a [[short-range forecast]] although  [[persistence]] and [[climatology]] are options, a forecast model, knowledge of the relative [[error]] of the  many different observational platforms employed as well as knowledge of the [[error]] in the [[background field|background  field]], and the spatial [[covariance]] of the various errors. [[real time|Real time]] computational considerations  generally limit the complexity of methods used. Historically important is the subjective  hand analysis, that is, drawing isobars on a map given [[mean sea level]] pressure at a set of observing  stations. Most analysis systems in the past have been at best 3D spatial analyses; time&ndash;space analysis  systems have recently emerged at operational [[prediction]] centers. A long series of analyses is of  great utility for studying the behavior of the atmospheric [[climate system]]. <br/>''See'' [[reanalysis]], [[variational objective analysis|variational  objective analysis]].
== analysis ==
}}
  </div>
}}
 
#<div class="definition"><div class="short_definition">In [[synoptic meteorology]], a detailed study of the state of the [[atmosphere]] based on  observations, usually including a separation of the entity into its component patterns and involving  the drawing of families of [[isopleths]] for various elements.</div><br/> <div class="paragraph">Thus, the analysis of [[synoptic]] charts may consist, for example, of the drawing and the interpretation  of the patterns of [[wind]], [[pressure]], pressure change, [[temperature]], [[humidity]], [[clouds]],  and [[hydrometeors]], all based on observations taken or [[forecast]] simultaneously.</div><br/> </div>
#<div class="definition"><div class="short_definition">A procedure to project the state of the [[atmosphere]] (or any system) as known from a finite  set of imperfect, irregularly distributed observations onto a regular [[grid]] or to represent the atmospheric  state by the [[amplitude]] of [[standard]] mathematical functions.</div><br/> <div class="paragraph">The grid and/or functional expansion allows for subsequent forecasts by [[numerical integration]]  or for easy diagnostic study. An analysis may be looked upon as a space&ndash;time [[interpolation]] system.  Essential ingredients of analysis are a [[background field]], usually a [[short-range forecast]] although  [[persistence]] and [[climatology]] are options, a forecast model, knowledge of the relative [[error]] of the  many different observational platforms employed as well as knowledge of the [[error]] in the [[background field|background  field]], and the spatial [[covariance]] of the various errors. [[real time|Real time]] computational considerations  generally limit the complexity of methods used. Historically important is the subjective  hand analysis, that is, drawing isobars on a map given [[mean sea level]] pressure at a set of observing  stations. Most analysis systems in the past have been at best 3D spatial analyses; time&ndash;space analysis  systems have recently emerged at operational [[prediction]] centers. A long series of analyses is of  great utility for studying the behavior of the atmospheric [[climate system]]. <br/>''See'' [[reanalysis]], [[variational objective analysis|variational  objective analysis]].</div><br/> </div>
</div>
 
{{TermIndex}}
{{TermFooter}}
 
[[Category:Terms_A]]

Latest revision as of 21:21, 13 January 2024

#In synoptic meteorology, a detailed study of the state of the atmosphere based on observations, usually including a separation of the entity into its component patterns and involving the drawing of families of isopleths for various elements.

Thus, the analysis of synoptic charts may consist, for example, of the drawing and the interpretation of the patterns of wind, pressure, pressure change, temperature, humidity, clouds, and hydrometeors, all based on observations taken or forecast simultaneously.

  1. A procedure to project the state of the atmosphere (or any system) as known from a finite set of imperfect, irregularly distributed observations onto a regular grid or to represent the atmospheric state by the amplitude of standard mathematical functions.
    The grid and/or functional expansion allows for subsequent forecasts by numerical integration or for easy diagnostic study. An analysis may be looked upon as a space–time interpolation system. Essential ingredients of analysis are a background field, usually a short-range forecast although persistence and climatology are options, a forecast model, knowledge of the relative error of the many different observational platforms employed as well as knowledge of the error in the background field, and the spatial covariance of the various errors. Real time computational considerations generally limit the complexity of methods used. Historically important is the subjective hand analysis, that is, drawing isobars on a map given mean sea level pressure at a set of observing stations. Most analysis systems in the past have been at best 3D spatial analyses; time–space analysis systems have recently emerged at operational prediction centers. A long series of analyses is of great utility for studying the behavior of the atmospheric climate system.
    See reanalysis, variational objective analysis.


Copyright 2024 American Meteorological Society (AMS). For permission to reuse any portion of this work, please contact permissions@ametsoc.org. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act (17 U.S. Code § 107) or that satisfies the conditions specified in Section 108 of the U.S.Copyright Act (17 USC § 108) does not require AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, require written permission or a license from AMS. Additional details are provided in the AMS Copyright Policy statement.