Sebastian Mernild - Academia.edu (original) (raw)
Papers by Sebastian Mernild
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The …, Jan 1, 2012
ABSTRACT The freshwater runoff from the glaciated and snow-covered Sermilik Fjord catchment, SE G... more ABSTRACT The freshwater runoff from the glaciated and snow-covered Sermilik Fjord catchment, SE Greenland, was estimated at annual resolution for the period 1900–2008 and at decadal resolution for the past four millennia. Our simulations were forced with available meteorological station data (1900–2008) and Greenland ice core estimated temperature data (1899 bc–ad 1980) from Dye3 and GISP2. Time series of estimated ice discharge (2000–2009) for the three major outlet glaciers Helheim, Fenris, and Midgård indicate that 53–74% of the ice discharge variations could be explained by variations in areally averaged glacier terminus surface (supraglacial) runoff. Based on these data and together with calculated subglacial geothermal and frictional melting as well as net precipitation for the fjord area, the Sermilik Fjord freshwater flux was deduced for the period 1900–2008. Our simulations indicated that during the last century surface freshwater runoff has equaled 13% of the Sermilik Fjord average freshwater flux of 33.0±5.7×109 m3/yr, covering a periodic runoff variation of 20 years. Ice discharge has accounted for 81%, with 63% of the freshwater flux originated from the Helheim glacier. This indicates that the Helheim outlet glacier plays a dominant role as a freshwater source to both Sermilik Fjord and ultimately the Irminger Sea. For the palaeorecords of the last 4000 years, simulated surface runoff has averaged 4.4±0.2×109 m3/yr. A very weak decreasing trend in runoff over the last 4 k years (1899 bc–ad 1980) is presumably associated with the general insolation-generated Northern Hemisphere cooling since the Holocene Thermal Maximum. Our simulations furthermore indicated centennial- to submillennial-scale variations in surface runoff concurrent with the well-known climate episodes such as the ‘Roman Warm Period’, the ‘Dark Ages Cold Period’, the ‘Medieval Climate Anomaly’, and the ‘Little Ice Age’. During the ‘Little Ice Age’, e.g., the average surface runoff was about 0.7×109 m3/yr lower than today, while the increase in runoff for the Modern Warming, since the late 1800s, was the second strongest and fastest for the last 4 k years.
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IAHS …, Jan 1, 2006
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Journal of Glaciology, Jan 1, 2011
Page 1. Greenland ice sheet surface melt extent and trends: 19602010 Sebastian H. MERNILD,1 Thom... more Page 1. Greenland ice sheet surface melt extent and trends: 19602010 Sebastian H. MERNILD,1 Thomas L. MOTE,2 Glen E. LISTON3 1Climate, Ocean and Sea Ice Modeling Group, Computational Physics and Methods, Los ...
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Eos Trans. AGU, Jan 1, 2009
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Journal of …, Jan 1, 2006
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Advances in Ecological …, Jan 1, 2008
At Zackenberg (74°30′N, 20°30′W), the polar night lasts 89 days and the polar day 106 days. Durin... more At Zackenberg (74°30′N, 20°30′W), the polar night lasts 89 days and the polar day 106 days. During the polar night, when solar energy is low or equal to zero, radiative cooling of the snow-covered surface leads to monthly mean air temperatures below −20 °C and daily ...
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Hydrological Processes, Jan 1, 2007
Page 1. HYDROLOGICAL PROCESSES Hydrol. Process. 21, 32493263 (2007) Published online 12 October ... more Page 1. HYDROLOGICAL PROCESSES Hydrol. Process. 21, 32493263 (2007) Published online 12 October 2007 in Wiley InterScience (www.interscience.wiley.com) DOI: 10.1002/hyp.6500 Snow-distribution and melt modelling for glaciers in ...
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Geografisk Tidsskrift-Danish Journal of …, Jan 1, 2006
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Journal of …, Jan 1, 2008
... SnowTran-3D simulations have previously been compared against observations in glacier and gla... more ... SnowTran-3D simulations have previously been compared against observations in glacier and glacier-free alpine, Arctic, and Antarctic ... Few quality observations for spatial in situ snow evolution, snow and ice surface melt, and glacier net mass balance are available. ...
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Hydrological …, Jan 1, 2009
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Hydrological Processes, Jan 1, 2008
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Hydrological Processes, Jan 1, 2008
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IAHS Publications-Series of …, Jan 1, 2004
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Hydrology …, Jan 1, 2008
RefDoc Bienvenue - Welcome. Refdoc est un service / is powered by. ...
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Journal of …, Jan 1, 2010
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Journal of Glaciology, Jan 1, 2009
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Journal of Applied Meteorology and …, Jan 1, 2010
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… Tidsskrift-Danish Journal …, Jan 1, 2008
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… Journal of Geography, Jan 1, 2004
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The …, Jan 1, 2012
ABSTRACT The freshwater runoff from the glaciated and snow-covered Sermilik Fjord catchment, SE G... more ABSTRACT The freshwater runoff from the glaciated and snow-covered Sermilik Fjord catchment, SE Greenland, was estimated at annual resolution for the period 1900–2008 and at decadal resolution for the past four millennia. Our simulations were forced with available meteorological station data (1900–2008) and Greenland ice core estimated temperature data (1899 bc–ad 1980) from Dye3 and GISP2. Time series of estimated ice discharge (2000–2009) for the three major outlet glaciers Helheim, Fenris, and Midgård indicate that 53–74% of the ice discharge variations could be explained by variations in areally averaged glacier terminus surface (supraglacial) runoff. Based on these data and together with calculated subglacial geothermal and frictional melting as well as net precipitation for the fjord area, the Sermilik Fjord freshwater flux was deduced for the period 1900–2008. Our simulations indicated that during the last century surface freshwater runoff has equaled 13% of the Sermilik Fjord average freshwater flux of 33.0±5.7×109 m3/yr, covering a periodic runoff variation of 20 years. Ice discharge has accounted for 81%, with 63% of the freshwater flux originated from the Helheim glacier. This indicates that the Helheim outlet glacier plays a dominant role as a freshwater source to both Sermilik Fjord and ultimately the Irminger Sea. For the palaeorecords of the last 4000 years, simulated surface runoff has averaged 4.4±0.2×109 m3/yr. A very weak decreasing trend in runoff over the last 4 k years (1899 bc–ad 1980) is presumably associated with the general insolation-generated Northern Hemisphere cooling since the Holocene Thermal Maximum. Our simulations furthermore indicated centennial- to submillennial-scale variations in surface runoff concurrent with the well-known climate episodes such as the ‘Roman Warm Period’, the ‘Dark Ages Cold Period’, the ‘Medieval Climate Anomaly’, and the ‘Little Ice Age’. During the ‘Little Ice Age’, e.g., the average surface runoff was about 0.7×109 m3/yr lower than today, while the increase in runoff for the Modern Warming, since the late 1800s, was the second strongest and fastest for the last 4 k years.
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IAHS …, Jan 1, 2006
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Journal of Glaciology, Jan 1, 2011
Page 1. Greenland ice sheet surface melt extent and trends: 19602010 Sebastian H. MERNILD,1 Thom... more Page 1. Greenland ice sheet surface melt extent and trends: 19602010 Sebastian H. MERNILD,1 Thomas L. MOTE,2 Glen E. LISTON3 1Climate, Ocean and Sea Ice Modeling Group, Computational Physics and Methods, Los ...
Bookmarks Related papers MentionsView impact
Eos Trans. AGU, Jan 1, 2009
Bookmarks Related papers MentionsView impact
Journal of …, Jan 1, 2006
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Advances in Ecological …, Jan 1, 2008
At Zackenberg (74°30′N, 20°30′W), the polar night lasts 89 days and the polar day 106 days. Durin... more At Zackenberg (74°30′N, 20°30′W), the polar night lasts 89 days and the polar day 106 days. During the polar night, when solar energy is low or equal to zero, radiative cooling of the snow-covered surface leads to monthly mean air temperatures below −20 °C and daily ...
Bookmarks Related papers MentionsView impact
Hydrological Processes, Jan 1, 2007
Page 1. HYDROLOGICAL PROCESSES Hydrol. Process. 21, 32493263 (2007) Published online 12 October ... more Page 1. HYDROLOGICAL PROCESSES Hydrol. Process. 21, 32493263 (2007) Published online 12 October 2007 in Wiley InterScience (www.interscience.wiley.com) DOI: 10.1002/hyp.6500 Snow-distribution and melt modelling for glaciers in ...
Bookmarks Related papers MentionsView impact
Geografisk Tidsskrift-Danish Journal of …, Jan 1, 2006
Bookmarks Related papers MentionsView impact
Journal of …, Jan 1, 2008
... SnowTran-3D simulations have previously been compared against observations in glacier and gla... more ... SnowTran-3D simulations have previously been compared against observations in glacier and glacier-free alpine, Arctic, and Antarctic ... Few quality observations for spatial in situ snow evolution, snow and ice surface melt, and glacier net mass balance are available. ...
Bookmarks Related papers MentionsView impact
Hydrological …, Jan 1, 2009
Bookmarks Related papers MentionsView impact
Hydrological Processes, Jan 1, 2008
Bookmarks Related papers MentionsView impact
Hydrological Processes, Jan 1, 2008
Bookmarks Related papers MentionsView impact
IAHS Publications-Series of …, Jan 1, 2004
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Hydrology …, Jan 1, 2008
RefDoc Bienvenue - Welcome. Refdoc est un service / is powered by. ...
Bookmarks Related papers MentionsView impact
Journal of …, Jan 1, 2010
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Journal of Glaciology, Jan 1, 2009
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Journal of Applied Meteorology and …, Jan 1, 2010
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… Tidsskrift-Danish Journal …, Jan 1, 2008
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… Journal of Geography, Jan 1, 2004
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