Integrative Remote Sensing Applications to Understanding Noctilucent Clouds and the Greenland Ice Sheet
Integrative remote sensing methods are effective in the study of large heterogeneous phenomena that contribute towards our understanding of global climatological trends. This study focuses upon two climatological subjects of integrative remote sensing techniques: glaciers and noctilucent clouds. Gla...
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ftunicolboulder:oai:scholar.colorado.edu:asen_gradetds-1030 2023-05-15T16:21:18+02:00 Integrative Remote Sensing Applications to Understanding Noctilucent Clouds and the Greenland Ice Sheet Reimuller, Jason David 2011-01-01T08:00:00Z application/pdf https://scholar.colorado.edu/asen_gradetds/29 https://scholar.colorado.edu/cgi/viewcontent.cgi?article=1030&context=asen_gradetds unknown CU Scholar https://scholar.colorado.edu/asen_gradetds/29 https://scholar.colorado.edu/cgi/viewcontent.cgi?article=1030&context=asen_gradetds Aerospace Engineering Sciences Graduate Theses & Dissertations airborne climate glacier mesospheric noctilucent remote sensing Aerospace Engineering text 2011 ftunicolboulder 2018-10-07T08:48:56Z Integrative remote sensing methods are effective in the study of large heterogeneous phenomena that contribute towards our understanding of global climatological trends. This study focuses upon two climatological subjects of integrative remote sensing techniques: glaciers and noctilucent clouds. Glaciers are considered among the most sensitive observable effects of climate change, whereas noctilucent clouds provide a means to observe the trends of a changing atmospheric composition. Through synchronized aircraft and spacecraft observations, this study verified for the first time that synchronous imagery of noctilucent cloud structures from airborne and spaceborne platforms could be obtained as similar band structures were identified, along with orthogonal structures only perceptible by the aircraft imagers. This helped to validate the processing algorithm at the day-to-night solar terminator of the Cloud Imagery and Particle Size (CIPS) instrument on the NASA Aeronomy of Ice in the Mesosphere (AIM) satellite. Furthermore, integrative methods were successful in determining the sliding component of glacial motion along the flowlines leading to the Sermeq Avannarleq glacier in Greenland and correlating this component to bedrock topography. Using a combination of airborne, spaceborne, and in-situ measurements, it was found that the initial onset of sliding occurs near the equilibrium line, quickly constituting approximately half of overall motion and increase steadily to the terminus, providing insight to positive feedback mechanisms that could accelerate glacial disintegration. Text glacier Greenland Ice Sheet University of Colorado, Boulder: CU Scholar Greenland Avannarleq ENVELOPE(-49.100,-49.100,62.133,62.133) Sermeq Avannarleq ENVELOPE(-50.833,-50.833,71.033,71.033) |
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Open Polar |
collection |
University of Colorado, Boulder: CU Scholar |
op_collection_id |
ftunicolboulder |
language |
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topic |
airborne climate glacier mesospheric noctilucent remote sensing Aerospace Engineering |
spellingShingle |
airborne climate glacier mesospheric noctilucent remote sensing Aerospace Engineering Reimuller, Jason David Integrative Remote Sensing Applications to Understanding Noctilucent Clouds and the Greenland Ice Sheet |
topic_facet |
airborne climate glacier mesospheric noctilucent remote sensing Aerospace Engineering |
description |
Integrative remote sensing methods are effective in the study of large heterogeneous phenomena that contribute towards our understanding of global climatological trends. This study focuses upon two climatological subjects of integrative remote sensing techniques: glaciers and noctilucent clouds. Glaciers are considered among the most sensitive observable effects of climate change, whereas noctilucent clouds provide a means to observe the trends of a changing atmospheric composition. Through synchronized aircraft and spacecraft observations, this study verified for the first time that synchronous imagery of noctilucent cloud structures from airborne and spaceborne platforms could be obtained as similar band structures were identified, along with orthogonal structures only perceptible by the aircraft imagers. This helped to validate the processing algorithm at the day-to-night solar terminator of the Cloud Imagery and Particle Size (CIPS) instrument on the NASA Aeronomy of Ice in the Mesosphere (AIM) satellite. Furthermore, integrative methods were successful in determining the sliding component of glacial motion along the flowlines leading to the Sermeq Avannarleq glacier in Greenland and correlating this component to bedrock topography. Using a combination of airborne, spaceborne, and in-situ measurements, it was found that the initial onset of sliding occurs near the equilibrium line, quickly constituting approximately half of overall motion and increase steadily to the terminus, providing insight to positive feedback mechanisms that could accelerate glacial disintegration. |
format |
Text |
author |
Reimuller, Jason David |
author_facet |
Reimuller, Jason David |
author_sort |
Reimuller, Jason David |
title |
Integrative Remote Sensing Applications to Understanding Noctilucent Clouds and the Greenland Ice Sheet |
title_short |
Integrative Remote Sensing Applications to Understanding Noctilucent Clouds and the Greenland Ice Sheet |
title_full |
Integrative Remote Sensing Applications to Understanding Noctilucent Clouds and the Greenland Ice Sheet |
title_fullStr |
Integrative Remote Sensing Applications to Understanding Noctilucent Clouds and the Greenland Ice Sheet |
title_full_unstemmed |
Integrative Remote Sensing Applications to Understanding Noctilucent Clouds and the Greenland Ice Sheet |
title_sort |
integrative remote sensing applications to understanding noctilucent clouds and the greenland ice sheet |
publisher |
CU Scholar |
publishDate |
2011 |
url |
https://scholar.colorado.edu/asen_gradetds/29 https://scholar.colorado.edu/cgi/viewcontent.cgi?article=1030&context=asen_gradetds |
long_lat |
ENVELOPE(-49.100,-49.100,62.133,62.133) ENVELOPE(-50.833,-50.833,71.033,71.033) |
geographic |
Greenland Avannarleq Sermeq Avannarleq |
geographic_facet |
Greenland Avannarleq Sermeq Avannarleq |
genre |
glacier Greenland Ice Sheet |
genre_facet |
glacier Greenland Ice Sheet |
op_source |
Aerospace Engineering Sciences Graduate Theses & Dissertations |
op_relation |
https://scholar.colorado.edu/asen_gradetds/29 https://scholar.colorado.edu/cgi/viewcontent.cgi?article=1030&context=asen_gradetds |
_version_ |
1766009309069574144 |