---
_id: '14885'
abstract:
- lang: eng
text: The near-surface boundary layer can mediate the response of mountain glaciers
to external climate, cooling the overlying air and promoting a density-driven
glacier wind. The fundamental processes are conceptually well understood, though
the magnitudes of cooling and presence of glacier winds are poorly quantified
in space and time, increasing the forcing uncertainty for melt models. We utilize
a new data set of on-glacier meteorological measurements on three neighboring
glaciers in the Swiss Alps to explore their distinct response to regional climate
under the extreme 2022 summer. We find that synoptic wind origins and local terrain
modifications, not only glacier size, play an important role in the ability of
a glacier to cool the near-surface air. Warm air intrusions from valley or synoptically-driven
winds onto the glacier can occur between ∼19% and 64% of the time and contribute
between 3% and 81% of the total sensible heat flux to the surface during warm
afternoon hours, depending on the fetch of the glacier flowline and its susceptibility
to boundary layer erosion. In the context of extreme summer warmth, indicative
of future conditions, the boundary layer cooling (up to 6.5°C cooler than its
surroundings) and resultant katabatic wind flow are highly heterogeneous between
the study glaciers, highlighting the complex and likely non-linear response of
glaciers to an uncertain future.
acknowledgement: This project has received funding from the European Union's Horizon
2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement
No. 101026058. The authors acknowledge the invaluable field assistance of Marta
Corrà, Achille Jouberton, Marin Kneib, Stefan Fugger, Celine Ducret and Alexander
Groos. The authors would also like to thank Luca Carturan for advice regarding AWS
setup and maintenance and Simone Fatichi for provision and support in the use of
the Tethys-Chloris model. Open access funding provided by ETH-Bereich Forschungsanstalten.
article_number: e2023JD040214
article_processing_charge: Yes (in subscription journal)
article_type: original
author:
- first_name: Thomas
full_name: Shaw, Thomas
id: 3caa3f91-1f03-11ee-96ce-e0e553054d6e
last_name: Shaw
orcid: 0000-0001-7640-6152
- first_name: Pascal
full_name: Buri, Pascal
id: 317987aa-9421-11ee-ac5a-b941b041abba
last_name: Buri
- first_name: Michael
full_name: Mccarthy, Michael
id: 22a2674a-61ce-11ee-94b5-d18813baf16f
last_name: Mccarthy
- first_name: Evan S.
full_name: Miles, Evan S.
last_name: Miles
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
orcid: 0000-0002-5554-8087
citation:
ama: 'Shaw T, Buri P, McCarthy M, Miles ES, Pellicciotti F. Local controls on near-surface
glacier cooling under warm atmospheric conditions. Journal of Geophysical Research:
Atmospheres. 2024;129(2). doi:10.1029/2023JD040214'
apa: 'Shaw, T., Buri, P., McCarthy, M., Miles, E. S., & Pellicciotti, F. (2024).
Local controls on near-surface glacier cooling under warm atmospheric conditions.
Journal of Geophysical Research: Atmospheres. Wiley. https://doi.org/10.1029/2023JD040214'
chicago: 'Shaw, Thomas, Pascal Buri, Michael McCarthy, Evan S. Miles, and Francesca
Pellicciotti. “Local Controls on Near-Surface Glacier Cooling under Warm Atmospheric
Conditions.” Journal of Geophysical Research: Atmospheres. Wiley, 2024.
https://doi.org/10.1029/2023JD040214.'
ieee: 'T. Shaw, P. Buri, M. McCarthy, E. S. Miles, and F. Pellicciotti, “Local controls
on near-surface glacier cooling under warm atmospheric conditions,” Journal
of Geophysical Research: Atmospheres, vol. 129, no. 2. Wiley, 2024.'
ista: 'Shaw T, Buri P, McCarthy M, Miles ES, Pellicciotti F. 2024. Local controls
on near-surface glacier cooling under warm atmospheric conditions. Journal of
Geophysical Research: Atmospheres. 129(2), e2023JD040214.'
mla: 'Shaw, Thomas, et al. “Local Controls on Near-Surface Glacier Cooling under
Warm Atmospheric Conditions.” Journal of Geophysical Research: Atmospheres,
vol. 129, no. 2, e2023JD040214, Wiley, 2024, doi:10.1029/2023JD040214.'
short: 'T. Shaw, P. Buri, M. McCarthy, E.S. Miles, F. Pellicciotti, Journal of Geophysical
Research: Atmospheres 129 (2024).'
date_created: 2024-01-28T23:01:42Z
date_published: 2024-01-28T00:00:00Z
date_updated: 2024-02-06T08:44:02Z
day: '28'
ddc:
- '550'
department:
- _id: FrPe
doi: 10.1029/2023JD040214
file:
- access_level: open_access
checksum: cad5b93caadb40c14e5faedc34f7bba7
content_type: application/pdf
creator: dernst
date_created: 2024-02-06T08:38:27Z
date_updated: 2024-02-06T08:38:27Z
file_id: '14943'
file_name: 2024_JGRAtmospheres_Shaw.pdf
file_size: 7481087
relation: main_file
success: 1
file_date_updated: 2024-02-06T08:38:27Z
has_accepted_license: '1'
intvolume: ' 129'
issue: '2'
language:
- iso: eng
month: '01'
oa: 1
oa_version: Published Version
publication: 'Journal of Geophysical Research: Atmospheres'
publication_identifier:
eissn:
- 2169-8996
issn:
- 2169-897X
publication_status: published
publisher: Wiley
quality_controlled: '1'
related_material:
record:
- id: '14919'
relation: research_data
status: public
scopus_import: '1'
status: public
title: Local controls on near-surface glacier cooling under warm atmospheric conditions
tmp:
image: /images/cc_by.png
legal_code_url: https://creativecommons.org/licenses/by/4.0/legalcode
name: Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)
short: CC BY (4.0)
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 129
year: '2024'
...
---
_id: '12583'
abstract:
- lang: eng
text: Peruvian glaciers are important contributors to dry season runoff for agriculture
and hydropower, but they are at risk of disappearing due to climate change. We
applied a physically based, energy balance melt model at five on-glacier sites
within the Peruvian Cordilleras Blanca and Vilcanota. Net shortwave radiation
dominates the energy balance, and despite this flux being higher in the dry season,
melt rates are lower due to losses from net longwave radiation and the latent
heat flux. The sensible heat flux is a relatively small contributor to melt energy.
At three of the sites the wet season snowpack was discontinuous, forming and melting
within a daily to weekly timescale, and resulting in highly variable melt rates
closely related to precipitation dynamics. Cold air temperatures due to a strong
La Niña year at Shallap Glacier (Cordillera Blanca) resulted in a continuous wet
season snowpack, significantly reducing wet season ablation. Sublimation was most
important at the highest site in the accumulation zone of the Quelccaya Ice Cap
(Cordillera Vilcanota), accounting for 81% of ablation, compared to 2%–4% for
the other sites. Air temperature and precipitation inputs were perturbed to investigate
the climate sensitivity of the five glaciers. At the lower sites warmer air temperatures
resulted in a switch from snowfall to rain, so that ablation was increased via
the decrease in albedo and increase in net shortwave radiation. At the top of
Quelccaya Ice Cap warming caused melting to replace sublimation so that ablation
increased nonlinearly with air temperature.
article_number: e2021JD034911
article_processing_charge: No
article_type: original
author:
- first_name: Catriona L.
full_name: Fyffe, Catriona L.
last_name: Fyffe
- first_name: Emily
full_name: Potter, Emily
last_name: Potter
- first_name: Stefan
full_name: Fugger, Stefan
last_name: Fugger
- first_name: Andrew
full_name: Orr, Andrew
last_name: Orr
- first_name: Simone
full_name: Fatichi, Simone
last_name: Fatichi
- first_name: Edwin
full_name: Loarte, Edwin
last_name: Loarte
- first_name: Katy
full_name: Medina, Katy
last_name: Medina
- first_name: Robert Å.
full_name: Hellström, Robert Å.
last_name: Hellström
- first_name: Maud
full_name: Bernat, Maud
last_name: Bernat
- first_name: Caroline
full_name: Aubry‐Wake, Caroline
last_name: Aubry‐Wake
- first_name: Wolfgang
full_name: Gurgiser, Wolfgang
last_name: Gurgiser
- first_name: L. Baker
full_name: Perry, L. Baker
last_name: Perry
- first_name: Wilson
full_name: Suarez, Wilson
last_name: Suarez
- first_name: Duncan J.
full_name: Quincey, Duncan J.
last_name: Quincey
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
citation:
ama: 'Fyffe CL, Potter E, Fugger S, et al. The energy and mass balance of Peruvian
Glaciers. Journal of Geophysical Research: Atmospheres. 2021;126(23). doi:10.1029/2021jd034911'
apa: 'Fyffe, C. L., Potter, E., Fugger, S., Orr, A., Fatichi, S., Loarte, E., …
Pellicciotti, F. (2021). The energy and mass balance of Peruvian Glaciers. Journal
of Geophysical Research: Atmospheres. American Geophysical Union. https://doi.org/10.1029/2021jd034911'
chicago: 'Fyffe, Catriona L., Emily Potter, Stefan Fugger, Andrew Orr, Simone Fatichi,
Edwin Loarte, Katy Medina, et al. “The Energy and Mass Balance of Peruvian Glaciers.”
Journal of Geophysical Research: Atmospheres. American Geophysical Union,
2021. https://doi.org/10.1029/2021jd034911.'
ieee: 'C. L. Fyffe et al., “The energy and mass balance of Peruvian Glaciers,”
Journal of Geophysical Research: Atmospheres, vol. 126, no. 23. American
Geophysical Union, 2021.'
ista: 'Fyffe CL, Potter E, Fugger S, Orr A, Fatichi S, Loarte E, Medina K, Hellström
RÅ, Bernat M, Aubry‐Wake C, Gurgiser W, Perry LB, Suarez W, Quincey DJ, Pellicciotti
F. 2021. The energy and mass balance of Peruvian Glaciers. Journal of Geophysical
Research: Atmospheres. 126(23), e2021JD034911.'
mla: 'Fyffe, Catriona L., et al. “The Energy and Mass Balance of Peruvian Glaciers.”
Journal of Geophysical Research: Atmospheres, vol. 126, no. 23, e2021JD034911,
American Geophysical Union, 2021, doi:10.1029/2021jd034911.'
short: 'C.L. Fyffe, E. Potter, S. Fugger, A. Orr, S. Fatichi, E. Loarte, K. Medina,
R.Å. Hellström, M. Bernat, C. Aubry‐Wake, W. Gurgiser, L.B. Perry, W. Suarez,
D.J. Quincey, F. Pellicciotti, Journal of Geophysical Research: Atmospheres 126
(2021).'
date_created: 2023-02-20T08:10:43Z
date_published: 2021-12-16T00:00:00Z
date_updated: 2023-02-28T13:31:08Z
day: '16'
doi: 10.1029/2021jd034911
extern: '1'
intvolume: ' 126'
issue: '23'
keyword:
- Space and Planetary Science
- Earth and Planetary Sciences (miscellaneous)
- Atmospheric Science
- Geophysics
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.1029/2021JD034911
month: '12'
oa: 1
oa_version: Published Version
publication: 'Journal of Geophysical Research: Atmospheres'
publication_identifier:
eissn:
- 2169-8996
issn:
- 2169-897X
publication_status: published
publisher: American Geophysical Union
quality_controlled: '1'
scopus_import: '1'
status: public
title: The energy and mass balance of Peruvian Glaciers
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 126
year: '2021'
...
---
_id: '9140'
abstract:
- lang: eng
text: 'Expected changes to future extreme precipitation remain a key uncertainty
associated with anthropogenic climate change. Extreme precipitation has been proposed
to scale with the precipitable water content in the atmosphere. Assuming constant
relative humidity, this implies an increase of precipitation extremes at a rate
of about 7% °C−1 globally as indicated by the Clausius‐Clapeyron relationship.
Increases faster and slower than Clausius‐Clapeyron have also been reported. In
this work, we examine the scaling between precipitation extremes and temperature
in the present climate using simulations and measurements from surface weather
stations collected in the frame of the HyMeX and MED‐CORDEX programs in Southern
France. Of particular interest are departures from the Clausius‐Clapeyron thermodynamic
expectation, their spatial and temporal distribution, and their origin. Looking
at the scaling of precipitation extreme with temperature, two regimes emerge which
form a hook shape: one at low temperatures (cooler than around 15°C) with rates
of increase close to the Clausius‐Clapeyron rate and one at high temperatures
(warmer than about 15°C) with sub‐Clausius‐Clapeyron rates and most often negative
rates. On average, the region of focus does not seem to exhibit super Clausius‐Clapeyron
behavior except at some stations, in contrast to earlier studies. Many factors
can contribute to departure from Clausius‐Clapeyron scaling: time and spatial
averaging, choice of scaling temperature (surface versus condensation level),
and precipitation efficiency and vertical velocity in updrafts that are not necessarily
constant with temperature. But most importantly, the dynamical contribution of
orography to precipitation in the fall over this area during the so‐called “Cevenoles”
events, explains the hook shape of the scaling of precipitation extremes.'
article_processing_charge: No
article_type: original
author:
- first_name: P.
full_name: Drobinski, P.
last_name: Drobinski
- first_name: B.
full_name: Alonzo, B.
last_name: Alonzo
- first_name: S.
full_name: Bastin, S.
last_name: Bastin
- first_name: N. Da
full_name: Silva, N. Da
last_name: Silva
- first_name: Caroline J
full_name: Muller, Caroline J
id: f978ccb0-3f7f-11eb-b193-b0e2bd13182b
last_name: Muller
orcid: 0000-0001-5836-5350
citation:
ama: 'Drobinski P, Alonzo B, Bastin S, Silva ND, Muller CJ. Scaling of precipitation
extremes with temperature in the French Mediterranean region: What explains the
hook shape? Journal of Geophysical Research: Atmospheres. 2016;121(7):3100-3119.
doi:10.1002/2015jd023497'
apa: 'Drobinski, P., Alonzo, B., Bastin, S., Silva, N. D., & Muller, C. J. (2016).
Scaling of precipitation extremes with temperature in the French Mediterranean
region: What explains the hook shape? Journal of Geophysical Research: Atmospheres.
American Geophysical Union. https://doi.org/10.1002/2015jd023497'
chicago: 'Drobinski, P., B. Alonzo, S. Bastin, N. Da Silva, and Caroline J Muller.
“Scaling of Precipitation Extremes with Temperature in the French Mediterranean
Region: What Explains the Hook Shape?” Journal of Geophysical Research: Atmospheres.
American Geophysical Union, 2016. https://doi.org/10.1002/2015jd023497.'
ieee: 'P. Drobinski, B. Alonzo, S. Bastin, N. D. Silva, and C. J. Muller, “Scaling
of precipitation extremes with temperature in the French Mediterranean region:
What explains the hook shape?,” Journal of Geophysical Research: Atmospheres,
vol. 121, no. 7. American Geophysical Union, pp. 3100–3119, 2016.'
ista: 'Drobinski P, Alonzo B, Bastin S, Silva ND, Muller CJ. 2016. Scaling of precipitation
extremes with temperature in the French Mediterranean region: What explains the
hook shape? Journal of Geophysical Research: Atmospheres. 121(7), 3100–3119.'
mla: 'Drobinski, P., et al. “Scaling of Precipitation Extremes with Temperature
in the French Mediterranean Region: What Explains the Hook Shape?” Journal
of Geophysical Research: Atmospheres, vol. 121, no. 7, American Geophysical
Union, 2016, pp. 3100–19, doi:10.1002/2015jd023497.'
short: 'P. Drobinski, B. Alonzo, S. Bastin, N.D. Silva, C.J. Muller, Journal of
Geophysical Research: Atmospheres 121 (2016) 3100–3119.'
date_created: 2021-02-15T14:21:16Z
date_published: 2016-03-16T00:00:00Z
date_updated: 2022-01-24T13:41:02Z
day: '16'
doi: 10.1002/2015jd023497
extern: '1'
intvolume: ' 121'
issue: '7'
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.1002/2015JD023497
month: '03'
oa: 1
oa_version: Published Version
page: 3100-3119
publication: 'Journal of Geophysical Research: Atmospheres'
publication_identifier:
issn:
- 2169-897X
- 2169-8996
publication_status: published
publisher: American Geophysical Union
quality_controlled: '1'
status: public
title: 'Scaling of precipitation extremes with temperature in the French Mediterranean
region: What explains the hook shape?'
type: journal_article
user_id: 8b945eb4-e2f2-11eb-945a-df72226e66a9
volume: 121
year: '2016'
...
---
_id: '12631'
abstract:
- lang: eng
text: Air temperature is one of the most relevant input variables for snow and ice
melt calculations. However, local meteorological conditions, complex topography,
and logistical concerns in glacierized regions make the measuring and modeling
of air temperature a difficult task. In this study, we investigate the spatial
distribution of 2 m air temperature over mountain glaciers and propose a modification
to an existing model to improve its representation. Spatially distributed meteorological
data from Haut Glacier d'Arolla (Switzerland), Place (Canada), and Juncal Norte
(Chile) Glaciers are used to examine approximate flow line temperatures during
their respective ablation seasons. During warm conditions (off-glacier temperatures
well above 0°C), observed air temperatures in the upper reaches of Place Glacier
and Haut Glacier d'Arolla decrease down glacier along the approximate flow line.
At Juncal Norte and Haut Glacier d'Arolla, an increase in air temperature is observed
over the glacier tongue. While the temperature behavior over the upper part can
be explained by the cooling effect of the glacier surface, the temperature increase
over the glacier tongue may be caused by several processes induced by the surrounding
warm atmosphere. In order to capture the latter effect, we add an additional term
to the Greuell and Böhm (GB) thermodynamic glacier wind model. For high off-glacier
temperatures, the modified GB model reduces root-mean-square error up to 32% and
provides a new approach for distributing air temperature over mountain glaciers
as a function of off-glacier temperatures and approximate glacier flow lines.
article_processing_charge: No
article_type: original
author:
- first_name: A.
full_name: Ayala, A.
last_name: Ayala
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
- first_name: J. M.
full_name: Shea, J. M.
last_name: Shea
citation:
ama: 'Ayala A, Pellicciotti F, Shea JM. Modeling 2 m air temperatures over mountain
glaciers: Exploring the influence of katabatic cooling and external warming. Journal
of Geophysical Research: Atmospheres. 2015;120(8):3139-3157. doi:10.1002/2015jd023137'
apa: 'Ayala, A., Pellicciotti, F., & Shea, J. M. (2015). Modeling 2 m air temperatures
over mountain glaciers: Exploring the influence of katabatic cooling and external
warming. Journal of Geophysical Research: Atmospheres. American Geophysical
Union. https://doi.org/10.1002/2015jd023137'
chicago: 'Ayala, A., Francesca Pellicciotti, and J. M. Shea. “Modeling 2 m Air Temperatures
over Mountain Glaciers: Exploring the Influence of Katabatic Cooling and External
Warming.” Journal of Geophysical Research: Atmospheres. American Geophysical
Union, 2015. https://doi.org/10.1002/2015jd023137.'
ieee: 'A. Ayala, F. Pellicciotti, and J. M. Shea, “Modeling 2 m air temperatures
over mountain glaciers: Exploring the influence of katabatic cooling and external
warming,” Journal of Geophysical Research: Atmospheres, vol. 120, no. 8.
American Geophysical Union, pp. 3139–3157, 2015.'
ista: 'Ayala A, Pellicciotti F, Shea JM. 2015. Modeling 2 m air temperatures over
mountain glaciers: Exploring the influence of katabatic cooling and external warming.
Journal of Geophysical Research: Atmospheres. 120(8), 3139–3157.'
mla: 'Ayala, A., et al. “Modeling 2 m Air Temperatures over Mountain Glaciers: Exploring
the Influence of Katabatic Cooling and External Warming.” Journal of Geophysical
Research: Atmospheres, vol. 120, no. 8, American Geophysical Union, 2015,
pp. 3139–57, doi:10.1002/2015jd023137.'
short: 'A. Ayala, F. Pellicciotti, J.M. Shea, Journal of Geophysical Research: Atmospheres
120 (2015) 3139–3157.'
date_created: 2023-02-20T08:16:28Z
date_published: 2015-04-18T00:00:00Z
date_updated: 2023-02-24T09:16:26Z
day: '18'
doi: 10.1002/2015jd023137
extern: '1'
intvolume: ' 120'
issue: '8'
keyword:
- Space and Planetary Science
- Earth and Planetary Sciences (miscellaneous)
- Atmospheric Science
- Geophysics
language:
- iso: eng
month: '04'
oa_version: Published Version
page: 3139-3157
publication: 'Journal of Geophysical Research: Atmospheres'
publication_identifier:
eissn:
- 2169-8996
issn:
- 2169-897X
publication_status: published
publisher: American Geophysical Union
quality_controlled: '1'
scopus_import: '1'
status: public
title: 'Modeling 2 m air temperatures over mountain glaciers: Exploring the influence
of katabatic cooling and external warming'
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 120
year: '2015'
...
---
_id: '12643'
abstract:
- lang: eng
text: Parameterizations of incoming longwave radiation are increasingly receiving
attention for both low and high elevation glacierized sites. In this paper, we
test 13 clear-sky parameterizations combined with seven cloud corrections for
all-sky atmospheric emissivity at one location on Haut Glacier d'Arolla. We also
analyze the four seasons separately and conduct a cross-validation to test the
parameters’ robustness. The best parameterization is the one by Dilley and O'Brien,
B for clear-sky conditions combined with Unsworth and Monteith cloud correction.
This model is also the most robust when tested in cross-validation. When validated
at different sites in the southern Alps of Switzerland and north-western Italian
Alps, all parameterizations show a substantial decrease in performance, except
for one site, thus suggesting that it is important to recalibrate parameterizations
of incoming longwave radiation for different locations. We argue that this is
due to differences in the structure of the atmosphere at the sites. We also quantify
the effect that the incoming longwave radiation parameterizations have on energy-balance
melt modeling, and show that recalibration of model parameters is needed. Using
parameters from other sites leads to a significant underestimation of melt and
to an error that is larger than that associated with using different parameterizations.
Once recalibrated, however, the parameters of most models seem to be stable over
seasons and years at the location on Haut Glacier d'Arolla.
article_processing_charge: No
article_type: original
author:
- first_name: I.
full_name: Juszak, I.
last_name: Juszak
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
citation:
ama: 'Juszak I, Pellicciotti F. A comparison of parameterizations of incoming longwave
radiation over melting glaciers: Model robustness and seasonal variability. Journal
of Geophysical Research: Atmospheres. 2013;118(8):3066-3084. doi:10.1002/jgrd.50277'
apa: 'Juszak, I., & Pellicciotti, F. (2013). A comparison of parameterizations
of incoming longwave radiation over melting glaciers: Model robustness and seasonal
variability. Journal of Geophysical Research: Atmospheres. American Geophysical
Union. https://doi.org/10.1002/jgrd.50277'
chicago: 'Juszak, I., and Francesca Pellicciotti. “A Comparison of Parameterizations
of Incoming Longwave Radiation over Melting Glaciers: Model Robustness and Seasonal
Variability.” Journal of Geophysical Research: Atmospheres. American Geophysical
Union, 2013. https://doi.org/10.1002/jgrd.50277.'
ieee: 'I. Juszak and F. Pellicciotti, “A comparison of parameterizations of incoming
longwave radiation over melting glaciers: Model robustness and seasonal variability,”
Journal of Geophysical Research: Atmospheres, vol. 118, no. 8. American
Geophysical Union, pp. 3066–3084, 2013.'
ista: 'Juszak I, Pellicciotti F. 2013. A comparison of parameterizations of incoming
longwave radiation over melting glaciers: Model robustness and seasonal variability.
Journal of Geophysical Research: Atmospheres. 118(8), 3066–3084.'
mla: 'Juszak, I., and Francesca Pellicciotti. “A Comparison of Parameterizations
of Incoming Longwave Radiation over Melting Glaciers: Model Robustness and Seasonal
Variability.” Journal of Geophysical Research: Atmospheres, vol. 118, no.
8, American Geophysical Union, 2013, pp. 3066–84, doi:10.1002/jgrd.50277.'
short: 'I. Juszak, F. Pellicciotti, Journal of Geophysical Research: Atmospheres
118 (2013) 3066–3084.'
date_created: 2023-02-20T08:17:34Z
date_published: 2013-04-27T00:00:00Z
date_updated: 2023-02-21T10:10:46Z
day: '27'
doi: 10.1002/jgrd.50277
extern: '1'
intvolume: ' 118'
issue: '8'
keyword:
- Space and Planetary Science
- Earth and Planetary Sciences (miscellaneous)
- Atmospheric Science
- Geophysics
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.1002/jgrd.50277
month: '04'
oa: 1
oa_version: Published Version
page: 3066-3084
publication: 'Journal of Geophysical Research: Atmospheres'
publication_identifier:
issn:
- 2169-897X
publication_status: published
publisher: American Geophysical Union
quality_controlled: '1'
scopus_import: '1'
status: public
title: 'A comparison of parameterizations of incoming longwave radiation over melting
glaciers: Model robustness and seasonal variability'
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 118
year: '2013'
...