First Passage Time Analysis on Climate Indices

Climate variability is simply represented by teleconnection patterns such as the Arctic Oscillation (AO), Antarctic Oscillation (AAO), North Atlantic Oscillation (NAO), Pacific/North American Pattern (PNA), and Southern Oscillation (SO) with associated indices Two approaches can be used to predict t...

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Main Author: Chu, Peter C.
Other Authors: NAVAL POSTGRADUATE SCHOOL MONTEREY CA NAVAL OCEAN ANALYSIS AND PREDICTION LAB
Format: Text
Language:English
Published: 2008
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA478896
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA478896
id ftdtic:ADA478896
record_format openpolar
spelling ftdtic:ADA478896 2023-05-15T13:58:29+02:00 First Passage Time Analysis on Climate Indices Chu, Peter C. NAVAL POSTGRADUATE SCHOOL MONTEREY CA NAVAL OCEAN ANALYSIS AND PREDICTION LAB 2008 text/html http://www.dtic.mil/docs/citations/ADA478896 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA478896 en eng http://www.dtic.mil/docs/citations/ADA478896 Approved for public release; distribution is unlimited. DTIC Meteorology *CLIMATE *PATTERNS FUNCTIONS TIME INTERVALS DENSITY INDEXES OSCILLATION SOUTH(DIRECTION) NORTH AMERICA ARCTIC REGIONS ANTARCTIC REGIONS BROWNIAN MOTION NORTH ATLANTIC OCEAN PACIFIC OCEAN FORWARD AREAS PREDICTIONS TIME SERIES ANALYSIS VARIATIONS Text 2008 ftdtic 2016-02-22T14:29:28Z Climate variability is simply represented by teleconnection patterns such as the Arctic Oscillation (AO), Antarctic Oscillation (AAO), North Atlantic Oscillation (NAO), Pacific/North American Pattern (PNA), and Southern Oscillation (SO) with associated indices Two approaches can be used to predict the indices: forward and backward methods The forward method is commonly used to predict the index fluctuation p at time t with a given temporal increment t Using this method% it was found that the index (such as for NAO) has the Brownian fluctuations On the base of the first passage time (FPT) concept, the backward method is introduced in this study to predict the typical time span (t) needed to generate a fluctuation in the index of a given increment p After the five monthly indices (AO, AAO, NAO, PNA, SO) running through the past history, the FPT density functions are obtained. FPT presents a new way to detect the temporal variability of the climate indices. The basic features for the index prediction are also discussed. Text Antarc* Antarctic Arctic North Atlantic North Atlantic oscillation Defense Technical Information Center: DTIC Technical Reports database Arctic Antarctic Pacific
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Meteorology
*CLIMATE
*PATTERNS
FUNCTIONS
TIME INTERVALS
DENSITY
INDEXES
OSCILLATION
SOUTH(DIRECTION)
NORTH AMERICA
ARCTIC REGIONS
ANTARCTIC REGIONS
BROWNIAN MOTION
NORTH ATLANTIC OCEAN
PACIFIC OCEAN
FORWARD AREAS
PREDICTIONS
TIME SERIES ANALYSIS
VARIATIONS
spellingShingle Meteorology
*CLIMATE
*PATTERNS
FUNCTIONS
TIME INTERVALS
DENSITY
INDEXES
OSCILLATION
SOUTH(DIRECTION)
NORTH AMERICA
ARCTIC REGIONS
ANTARCTIC REGIONS
BROWNIAN MOTION
NORTH ATLANTIC OCEAN
PACIFIC OCEAN
FORWARD AREAS
PREDICTIONS
TIME SERIES ANALYSIS
VARIATIONS
Chu, Peter C.
First Passage Time Analysis on Climate Indices
topic_facet Meteorology
*CLIMATE
*PATTERNS
FUNCTIONS
TIME INTERVALS
DENSITY
INDEXES
OSCILLATION
SOUTH(DIRECTION)
NORTH AMERICA
ARCTIC REGIONS
ANTARCTIC REGIONS
BROWNIAN MOTION
NORTH ATLANTIC OCEAN
PACIFIC OCEAN
FORWARD AREAS
PREDICTIONS
TIME SERIES ANALYSIS
VARIATIONS
description Climate variability is simply represented by teleconnection patterns such as the Arctic Oscillation (AO), Antarctic Oscillation (AAO), North Atlantic Oscillation (NAO), Pacific/North American Pattern (PNA), and Southern Oscillation (SO) with associated indices Two approaches can be used to predict the indices: forward and backward methods The forward method is commonly used to predict the index fluctuation p at time t with a given temporal increment t Using this method% it was found that the index (such as for NAO) has the Brownian fluctuations On the base of the first passage time (FPT) concept, the backward method is introduced in this study to predict the typical time span (t) needed to generate a fluctuation in the index of a given increment p After the five monthly indices (AO, AAO, NAO, PNA, SO) running through the past history, the FPT density functions are obtained. FPT presents a new way to detect the temporal variability of the climate indices. The basic features for the index prediction are also discussed.
author2 NAVAL POSTGRADUATE SCHOOL MONTEREY CA NAVAL OCEAN ANALYSIS AND PREDICTION LAB
format Text
author Chu, Peter C.
author_facet Chu, Peter C.
author_sort Chu, Peter C.
title First Passage Time Analysis on Climate Indices
title_short First Passage Time Analysis on Climate Indices
title_full First Passage Time Analysis on Climate Indices
title_fullStr First Passage Time Analysis on Climate Indices
title_full_unstemmed First Passage Time Analysis on Climate Indices
title_sort first passage time analysis on climate indices
publishDate 2008
url http://www.dtic.mil/docs/citations/ADA478896
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA478896
geographic Arctic
Antarctic
Pacific
geographic_facet Arctic
Antarctic
Pacific
genre Antarc*
Antarctic
Arctic
North Atlantic
North Atlantic oscillation
genre_facet Antarc*
Antarctic
Arctic
North Atlantic
North Atlantic oscillation
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA478896
op_rights Approved for public release; distribution is unlimited.
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