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Genthon,
C., M. S. Town, D. Six, V. Favier, S. Argentini, and A.
Pellegrini, 2010. Meteorological atmospheric boundary layer
measurements and ECMWF analyses during summer at Dome C,
Antarctica, J. Geophys. Res., 115, D05104,
doi:10.1029/2009JD012741.
Abstract:
Six levels of
meteorological sensors have been deployed along a 45 m tower at
the French-Italian Concordia station, Dome C, Antarctic. We
present measurements of vertical profiles, the diurnal cycle, and
interdiurnal variability of temperature, humidity, and wind speed
and direction for 3 weeks during the southern summer of 2008.
These measurements are compared to 6-hourly European Center for
Medium-Range Forecasts (ECMWF) analyses and daily radiosoundings.
The ECMWF analyses show a 3–4C warm bias relative to the tower
observations. They reproduce the diurnal cycle of temperature with
slightly weaker amplitude and weaker vertical gradients. The
amplitude of the diurnal cycle of relative humidity is
overestimated by ECMWF because the amplitude of the absolute
humidity diurnal cycle is too small. The nighttime surface-based
wind shear and Ekman spiral is also not reproduced in the ECMWF
analyses. Radiosonde temperatures are biased low relative to the
tower observations in the lowest 30 m but approach agreement at
the top of the tower. Prior to bias correction for age-related
contamination, radiosonde relative humidities are biased low
relative to the tower observations in the lowest 10 m but agree
with tower observations above this height. After correction for
the age-related bias, the radiosonde relative humidity agrees with
tower observations below 10 m but is biased high above this
height. Tower temperature observations may also be biased by solar
heating, despite radiation shielding and natural ventilation.
Rabier,
F., A. Bouchard, E. Brun, A. Doerenbecher, S. Guedj, V. Guidard,
F. Karbou, V.H. Peuch, L. El Amraoui, D. Puech, C. Genthon, G.
Picard, M. Town, A. Hertzog, F. Vial, P. Cocquerez, S.A. Cohn, T.
Hock, J. Fox, H. Cole, D. Parsons, J. Powers, K. Romberg, J.
VanAndel, T. Deshler, J. Mercer, J.S. Haase, L. Avallone, L.
Kalnajs, C.R. Mechoso, A. Tangborn, A. Pellegrini, Y. Frenot, J.N.
Thépaut, A. McNally, G. Balsamo, and P. Steinle, 2010. The
Concordiasi Project in Antarctica, Bull. Amer. Meteor. Soc., 91,
69–86. Open access!
Bellot,
H., F. A. Trouvilliez, F. Naaim-Bouvet, C. Genthon, H. Gallée,
201. Present weather sensors tests for measuring drifting snow,
Ann. Glaciol., vol. 52, n° 58, p. 176 – 184.
Agosta,
C., V. Favier, C. Genthon, H. Gallée, G. Krinner, J. Lenaerts, M.
R. van den Broeke, 2011. A 40-year surface accumulation dataset in
Adélie Land coastal area (66°S, 139°E) and its application for
atmospheric model validation, Clim. Dyn., doi:
10.1007/s00382-011-1103-4.
Favier
V. , C. Agosta, C. Genthon, L. Arnaud, A. Trouvilliez, 2011.
Modeling the mass and surface heat budgets in a coastal blue ice
area of Adelie Land, Antarctica, J. Geophys. Res., 116, F03017,
doi:10.1029/2010JF001939.
Brun,
E., D. six, G. Picard, V. Vionnet, L; Arnaud, E. Bazile, A. Boone,
O. Bouchard, C. Genthon, V. Guidard, P. Le Moigne, F. Rabier, Y.
Seity, 2011. Snow-atmosphere coupled simulation at Dome C,
Antarctica, J. Glaciol., 52(204), 721.
Genthon,
C., D. Six, V. Favier, M. Lazzara, L. Keller, 2011. Atmospheric
temperature measurement biases on the Antarctic plateau, Atm.
Oceanic Technol., DOI 10.1175/JTECH-D-11-00095.1, Vol. 28, No. 12,
1598-1605.
Abstract:
Observations of atmospheric
temperature made on the Antarctic plateau with thermistors housed
in naturally (wind) ventilated radiation shields are shown to be
significantly warm biased by solar radiation. High incoming solar
flux and high surface albedo result in radiation biases in Gill
(multiplate) styled shields that can occasionally exceed 10°C in
summer in case of low wind speed. Although stronger and more
frequent when incoming solar radiation is high, biases exceeding
8°C are found even when solar is less than 200 Wm-2. Comparing
with sonic thermometers, which are not affected by radiation but
which are too complex to be routinely used for mean temperature
monitoring, commercially available aspirated shields are shown to
efficiently protect thermistor measurements from solar radiation
biases. Most of the available in situ reports of atmospheric
temperature on the Antarctic plateau are from automatic weather
stations that use passive shields and are thus likely warm biased
in the summer. In spite of low power consumption, deploying
aspirated shields at remote locations in such a difficult
environment may be a challenge. Bias correction formulae are not
easily derived and are obviously shield dependent. On the other
hand, because of a strong dependence of bias to wind speed,
filtering out temperature reports for wind speed less than a given
threshold (about 4-6 ms-1 for the shields tested here) may be an
efficient way to quality control the data, albeit at the cost of
significant data loss and records biased towards high wind speed
cases.
Genthon,
C., A. Trouvilliez, H. Gallée, H. Bellot, F. Naaim, V. Favier, L.
Piard, 2011. Blizzard, très blizzard, La Météorologie, 75,
november 2011.
Abstract:
Twenty five years ago, a
field campaign was designed to observe an analyze the catabatic
winds of Adélie Land, a region where these winds are particularly
strong and persistent. Impressed by one major consequence of the
winds, the investigators then tagged Adélie Land, the Blizzard
Kingdom. Since 2009, with support from the french polar institute
and the European framework program for research, the CNRS and
CEMAGREF in Grenoble deploy and maintain instruments in Adélie
Land to measure blowing snow, increase our understanding of the
processes involved, improve blowing snow modeling, and better
assess the contribution of blowing snow to surface accumulation.
If Antarctic snow accumulation changes in response to climate
change, this will have global consequences on global sea-level.
Ricaud,
P., C. Genthon, J.-L. Attié, J.-F. Vanacker, L. Moggio, Y.
Courcoux, A. Pellegrini, and T. Rose, 2012. Summer to winter
variabilities of temperature and water vapor in the surface
atmosphere as observed by HAMSTRAD over Dome C, Antarctica, Bound.
Layer Met., 143, 227-259.
Gallée
H., Trouvilliez A., Agosta C., Genthon C., Favier V., and
Naaim-Bouvet F., 2011. Transport of snow by the wind: a comparison
between observations made in Adélie Land, Antarctica, and
simulations made with the Regional Climate Model MAR, Bound.
Layer. Met., DOI 10.1007/s10546-012-9764-z
http://www.springerlink.com/openurl.asp?genre=article&id=doi:10.1007/s10546-012-9764-z
<http://www.springer.com/alert/urltracking.do?id=Ld57cfeMab04ffSaa569b5>.
Open access!
Abstract:
For the first time a
simulation of blowing snow events was validated in detail using
one-month long observations (January 2010) made in Adélie Land,
Antarctica. A regional climate model featuring a coupled
atmosphere / blowing snow / snowpack model is forced laterally by
meteorological re-analyses. The vertical grid spacing ranged from
2 m to 20 m above the surface and the horizontal grid spacing was
5 km. The simulation was validated by comparing the occurrence of
blowing snow events and other meteorological parameters at two
automatic weather stations. The Nash test allowed us to compute
efficiencies of the simulation. The regional climate model
simulated the observed wind speed with a positive efficiency
(0.69). Wind speeds higher than 12 m s-1 were underestimated.
Positive efficiency of the simulated wind speed was a prerequisite
for validating the blowing snow model. Temperatures were simulated
with a slightly negative efficiency (--0.16) due to overestimation
of the amplitude of the diurnal cycle during one week, probably
because the cloud cover was underestimated at that location during
the period concerned. Snowfall events were correctly simulated by
our model, as confirmed by field reports. Because observations
suggested that our instrument (an acoustic sounder) tends to
overestimate the blowing snow flux, data were not sufficiently
accurate to allow the complete validation of snow drift values.
However, the simulation of blowing snow occurrence was in good
agreement with the observations made during the first 20 days of
January 2010, despite the fact that the blowing snow flux may be
underestimated by the regional climate model during pure blowing
snow events. We found that blowing snow occurs in Adélie Land
only when the half-hourly wind speed value at 2 m a.g.l. is higher
than 10 m s-1 . The validation for the last 10 days of January
2010 was less satisfactory because of complications introduced by
surface melting and refreezing.
Genthon
C., D. Six, H. Gallée, P. Grigioni, et A. Pellegrini, 2012. Two
years of atmospheric boundary layer observation on a 45-m tower at
Dome C, Antarctic plateau, J. Geophys. Res., in
press.
Abstract:
The lower atmospheric boundary
layer at Dome C on the Antarctic plateau is continuously monitored
along a 45-m tower since 2009. Years 2009 and 2010 are presented.
A strong diurnal cycle is observed near the surface in summer,
which is almost muted at the top of the tower, reflecting that the
summer nocturnal inversion is very shallow. Very steep inversions
reaching almost 1°C m-1 on average along the tower are observed
in winter. The inversions are stronger and more frequent during
the colder 2010 winter. The strongest inversions occur in a layer
~10-15 m above surface, locally reaching more than 2.5°C m-1.
Winter temperature is characterized by strong synoptic
variability. An extreme warm event occurred in full winter in July
2009 during which the temperature reached -30°C, typical of
mid-summer weather. The meteorological analyzes, which agree with
the observations near the surface, confirm that heat propagated
downward from the higher elevations. High total water column sign
warm and moist air mass in the free atmosphere originating from
the lower latitudes. Colder temperatures and stronger inversions
are conversely associated with a very dry atmosphere, particularly
in the colder winter 2010. Measurement of atmospheric moisture in
the clean and cold Antarctic plateau atmosphere is challenging.
Supersaturations are very likely but they are not reflected in the
tower observations. This is likely an instrumental artifact,
probably affecting other moisture reports from other measurements
in similar conditions.
Agosta,
C., V. Favier, G. Krinner, H. Gallée, et C. Genthon, 2013.
High-resolution modeling of the Antarctic surface mass balance,
application for the 20th and 21st centuries, Clim. Dyn., Vol 41
(11-12), 3247-3260 DOI: 10.1007/s00382-013-1903-9
Ricaud,
P., F. Carminati, J.-L. Attié, Y. Courcoux, T. Rose, C. Genthon,
A. Pellegrini, P. Tremblin, and T. August, 2013. Quality
Assessment of the First Measurements of Tropospheric Water Vapor
and Temperature by the HAMSTRAD Radiometer over Concordia Station,
Antarctica, IEEE TGRS, 51, 3217-3239.
Argentini,
S., I. Petenko, E. Viola, G. Mastrantonio, I. Pietroni, G.
Csasasanta, E. Artistidi, et C. Genthon, 2013. The surface layer
observed by a high resolution SODAR at Dome C, Antarctica, Annals
of Geophysics, 56, 1-10.
Ricaud,
P, F. Carminati, Y. Courcoux, A. Pellegrini, J.-L. Attié, L. El
Amraoui, C. Genthon, T. August, et J. Warner, 2014. Statistical
analyzes and correlation between tropospheric temperature and
humidity at Dome C, Antarctic Science,
doi:10.1017/S0954102013000564
Naaim-Bouvet,
F., H. bellot, K. Nishimura, C. Genthon, C. Palerme, G.
Guyomarc'h, et V. Vionnet, 2014. Detection of snow fall occurrence
during blowing snow events by photoelectric sensors, Cold Reg.
Sci. Technol. 106, 11-21.
Palerme,
C., J. E. Kay, C. Genthon, T. l'Ecuyer, N. B. Wood, et C. Claud,
2014. How much snow falls over the Antarctic ice sheet? The
Cryosphere, 8, 1577-1587, doi:10.5194/tc-8-1577-2014. Open
access!
Abstract :
Climate models predict
Antarctic precipitation to increase during the 21st century, but
their present day Antarctic precipitation differs. A
model-independent climatology of the Antarctic precipitation
characteristics, such as snowfall rates and frequency, is needed
to assess the models, but it is not yet available. Satellite
observations of precipitation by active sensors has been possible
in the polar regions since the launch of CloudSat in 2006. Here,
we use two CloudSat products to generate the first multi-year,
model-independent climatology of Antarctic precipitation. The
first product is used to determine the frequency and the phase of
precipitation, while the second product is used to assess the
snowfall rate. The mean snowfall rate from August 2006 to April
2011 is 171 mm year−1 over the Antarctic ice sheet, north of 82◦
S. While uncertainties on individual precipitation retrievals from
CloudSat data are potentially large, the mean uncertainty should
be much smaller, but cannot be easily estimated. There are no in
situ measurements of Antarctic precipitation to directly assess
the new climatology. However, distributions of both precipitation
occurrences and rates generally agree with the European Centre for
Medium-Range Weather Forecasts (ECMWF) ERA-Interim data set, the
production of which is constrained by various in situ and
satellite observations, but does not use any data from CloudSat.
The new data set thus offers unprecedented capability to
quantitatively assess Antarctic precipitation statistics and rates
in climate models.
Trouvilliez,
A., F. Naaim-Bouvet, C. Genthon, L. Piard, V. Favier, H. Bellot,
C. Agosta, C. Palerme, C. Amory, et H. Gallée, 2014. A novel
experimental study of aeolian snow transport in Adelie
Land(Antarctica), Cold Reg. Sci. Technol. 108, 125-138.
Barral,
H., C. Genthon, A. Trouvilliez, C. Brun, C. Amory, 2014. Blowing
snow in coastal Adélie Land, Antarctica : three atmospheric
moisture issues, The Cryosphere, 8, 1905–1919,
doi:10.5194/tc-8-1905-2014. Open access!
Abstract :
A
total of 3 years of blowing-snow observations and associated
meteorology along a 7 m mast at site D17 in coastal Adélie Land
are presented. The observations are used to address three
atmospheric-moisture issues related to the occurrence of blowing
snow, a feature which largely affects many regions of Antarctica:
(1) blowing-snow sublimation raises the moisture content of the
surface atmosphere close to saturation, and atmospheric models and
meteorological analyses that do not carry blowing-snow
parameterizations are affected by a systematic dry bias; (2) while
snowpack modelling with a parameterization of surface-snow erosion
by wind can reproduce the variability of snow accumulation and
ablation, ignoring the high levels of atmospheric-moisture content
associated with blowing snow results in overestimating surface
sublimation, affecting the energy budget of the snowpack; (3) the
well-known profile method of calculating turbulent moisture fluxes
is not applicable when blowing snow occurs, because moisture
gradients are weak due to blowing-snow sublimation, and the impact
of measurement uncertainties are strongly amplified in the case of
strong winds.
Genthon,
C., D. Six, C. Scarchilli, V. Giardini, M. Frezzotti, 2014.
Meteorological and snow accumulation gradients across dome C, east
Antarctic plateau, Int. J. Clim., DOI: 10.1002/joc.4362.
Absract:
In situ observations show that snow accumulation is
∼10% larger 25 km north than south of the summit of Dome C on
the east antarctic plateau. The mean wind direction is southerly.
Although a slight slope-related diverging katabatic flow component
is detectable, the area is an essentially flat (∼10 m elevation
change or less) homogeneous snow surface. The European Center for
Medium-range Weather Forecasts meteorological analyses data
reproduce a significant accumulation gradient and suggest that 90%
of the the mean accumulation results from the 25% largest
precipitation events. During these events, air masses originate
from coastal areas in the north rather than from inland in the
south. Radiative cooling condensation occurs on the way across the
dome and as the moisture reservoir is depleted less snow is dumped
25 km south than north, with little direct impact from the local
(50-km scale) topography. Air masses are warmer on average, and
warmer north than south, when originating from the coast. This
marginally affects the mean temperature gradients. The moisture
gradients are more affected because moisture is nonlinearly
related to temperature: the mean atmospheric moisture is larger
north than south. Significant meteorological and hydrological
gradients over such relatively small distances (50 km) over
locally flat region may be an issue when interpreting ice cores:
although cores are drilled at the top of domes and ridges where
the slopes and elevation gradients are minimal, they sample small
surfaces in areas affected by significant meteorological and
hydrological spatial gradients.
Gallée,
H., S. Preunkert, S. Argentini, M. M. Frey, C. Genthon, B.
Jourdain, I. Pietroni, G. Casasanta, H. Barral, E. Vignon, and M.
Legrand, 2015. Characterization of the boundary layer at Dome C
(East Antarctica) during the OPALE summer campaign, Atmos. Chem.
Phys., 15, 6225-6236, doi:10.5194/acp-15-6225.
Gallée,
H., H. Barral, E. Vignon, et C. Genthon, 2015. A case study of a
low level jet during OPALE, Atmos. Chem. Phys. 15, 6237-6246,
doi:10.5194/acp-15-6237-2015, 2015.
Amory,
C., A. Trouvilliez, H. Gallée, F. Naaim-Bouvet, C. Genthon, V.
favier, C. Agosta, L. Piard, et H. bellot, 2014. Comparison of
aeolian snow transport events and snow mass fluxes between
observations and simulations made by the regional climate model
MAR in Adélie Land, East Antarctica, The Cryosphere, 9,
1373-1383, doi:10.5194/tc-9-1373-2015. Open eccess!
Rysman,
J.F., S. Verrier, A. Lahellec, et C. Genthon, 2015. Analysis of
boundary layer statistical properties at Dome C, Antarctica,
Bound. Layer Met., Bound. Layer Met., 156, 145-155.
Casado,
M. A. Landais, V. Masson-Delmotte, C. Genthon, E. Kerstel, S.
Kassi, L. Arnaud, G. Picard, F. Prie, O. Cattani, H.-C.
Steen-Larsen, E. Vignon, and P. Cermak, 2016. Continuous
measurements of isotopic composition of water vapour on the East
Antarctic Plateau, Atm. Chem. Phys., 16, 8521-8538,
doi:10.5194/acp-16-8521-2016. Open access!
Casado,
M., A. Landais, G. Picard, T. Münch, T. Laepple, B. Stenni, G.
Dreossi, A. Ekaykin, L. Arnaud, C. Genthon, A. Touzeau, V.
Masson-Delmotte, J. and Jouzel, 2016. Archival of the water stable
isotope signal in East Antarctic ice cores. The Cryosphere,
doi:10.5194/tc-2016-263. Open access!
/mnt/genthonc/www-user/SiteCALVA
Vignon,
E., C. Genthon, H. barral, C. Amory, G. Casasanta, H. Gallée, F.
Hourdin, S. Argentini, and G. Picard, 2016. Surface turbulent
fluxes calculation over the Antarctic plateau: sensitivity to four
surface layers features, Bound. Lay. Met.., 162 (2):341-367, doi
10.1007/s10546-016-0192-3.
Vignon,
E. B. van de Wiel, I. van Hooijdonk, C. Genthon, S. van der
Linden, A. van Hooft, P. Baas, W. Maurel, and O. Traullé, 2016.
Stable Boundary Layer regimes at Dome C, Antarctica, QJRMS, 143,
1241-1253, DOI: 10.1002/qj.2998.
Van
de Wiel, B. J. H., E. Vignon, P. Baas, I.G.S. van Hooijdonk,
S.J.A. van der Linden, J. A. van Hooft, F.C. Bosveld, S.R. de
Roode, A.F. Moene, and C. Genthon, 2017. Regime transitions in
near-surface temperature inversions: a conceptual model”, J.
Atmos. Sci., 74, 1057-1073, DOI: 10.1175/JAS-D-16-0180.1
Amory,
C., H. Gallée, F. Naaim-Bouvet, E. Vignon, V. Favier, G. Picard,
A. Trouvilliez, L. Piard, C. Genthon, and H. Bellot, 2017.
Seasonal variations in drag coefficients over a sastrugi-covered
snowfield of coastal East Antarctica, Bound. Lay. Met.,
DOI:10.1007/s10546-017-0242-5.
Genthon,
C., L. Piard, E. Vignon, J.-B. Madeleine, M. Casado, H. Gallée,
2017. Atmospheric moisture supersaturation in the near-surface
atmosphere at Dome C, antarctic plateau, Atm. Phys. Chem., 17,
691-704, doi:10.5194/acp-17-691-2017. Open access!
Abstract
:
Supersaturation often occurs at the top of the troposphere
where cirrus clouds form, but is comparatively unusual near the
surface where the air is generally warmer and laden with liquid
and/or ice condensation nuclei. One exception is the surface of
the high Antarctic Plateau. One year of atmospheric moisture
measurement at the surface of Dome C on the East Antarctic Plateau
is presented. The measurements are obtained using commercial
hygrometry sensors modified to allow air sampling without
affecting the moisture content, even in the case of
supersaturation. Supersaturation is found to be very frequent.
Common unadapted hygrometry sensors generally fail to report
supersaturation, and most reports of atmospheric moisture on the
Antarctic Plateau are thus likely biased low. The measurements are
compared with results from two models implementing cold
microphysics parameterizations: the European Center for
Medium-range Weather Forecasts through its operational analyses,
and the Model Atmosphérique Régional. As in the observations,
supersaturation is frequent in the models but the statistical
distribution differs both between models and observations and
between the two models, leaving much room for model improvement.
This is unlikely to strongly affect estimations of surface
sublimation because supersaturation is more frequent as
temperature is lower, and moisture quantities and thus water
fluxes are small anyway. Ignoring supersaturation may be a more
serious issue when considering water isotopes, a tracer of phase
change and temperature, largely used to reconstruct past climates
and environments from ice cores. Because observations are easier
in the surface atmosphere, longer and more continuous in situ
observation series of atmospheric supersaturation can be obtained
than higher in the atmosphere to test parameterizations of cold
microphysics, such as those used in the formation of high-altitude
cirrus clouds in meteorological and climate models.
Palerme,
C., C. Claud, A. Dufour, C.
Genthon, J. Kay, N. Wood, T.
L'Ecuyer, 2017.
Evaluation of Antarctic snowfall in global meteorological
reanalyses, Atm. Res., 48 (1-2):225-239;, DOI
10.1007/s00382-016-3071-1.
Vignon,
E. , F. Hourdin, C. Genthon, H. Gallée, E. Bazile, M.-P.
Lefebvre, J.-B. Madeleine, and B. J. H. Van de Wiel, 2017.
Parametrization of surface and boundary-layer processes in a
General Circulation Model over the Antarctic Plateau: evaluation
of 1D simulations against clear-sky summertime
observations
from Dome C, J. Geophys. Res., 122, doi:10.1002/2017JD026802.
Grazioli,
J., C.
Genthon, B. Boudevillain, C.
Duran-Alarcon, M. Del Guasta, J.-B. Madeleine, et A.
Berne, 2017. Measurements of precipitation in
Dumont d’Urville, Terre Adélie, East Antarctica, The
Cryosphere, 11, 1797-1811, DOI:10.5194/tc-11-1797-2017
Grazioli,
J, J.-B. Madeleine, H. Gallee, R. M. Forbes, C. Genthon, G.
Krinner, and A. Berne, 2017. Katabatic winds diminish
precipitation contribution to the Antarctic ice mass balance,
PNAS, DOI:
10.1073/pnas.170763311.
Vignon,
E., F. hourdin, C. Genthon, B. van de Wiel, H. Gallée, J.-B.
Madeleine, eand J. baumet, 2017. Modeling the dynamics of the
Atmospheric Boundary Layer over the Antarctic Plateau with a
General Circulation Model, JAMES, 10, 98–125.
https://doi.org/10.1002/2017MS001184
Casado,
M., A. Landais, G. Picard, T. Münch, T. Laepple, B. Stenni, G.
Dreossi, A. Ekaykin, L. Arnaud, C. Genthon, A. Touzeau, V.
Masson-Delmotte, et
J.
Jouzel, 2018. Archival of the water stable isotope signal in East
Antarctic ice cores, The Cryosphere, 12, 1745-1766,
https://doi.org/10.5194/tc-12-1745-2018
Genthon,
C., R. Forbes, E. Vignon, A. Gettelman, and J.-B. Madeleine,
2018.Comment
on “Surface air relative humidities spuriously exceeding 100% in
CMIP5 model output and their impact on future projections” by
Ruosteenoja, Jylhä, Rälsänen and Mäkelä [2017], J. Geophys.
Res. Atm., . Geophys. Res. Atm., doi:10.1029/2017JD028111.
Genthon,
C., A. Berne, J. Grazioli, C. Durán
Alarcón,
C. Praz, B. Boudevillain, 2018. Precipitation at Dumont d'Urville,
Adélie Land, East Antarctica: the APRES3 campaigns dataset, Earth
Syst. Sci. Data, 10, 1–8, 2018,
https://doi.org/10.5194/essd-10-1-2018.
Palerme,
C., C. Claud, N. Wood, T. L’Ecuyer, C. Genthon,
2018.
How does ground clutter affect CloudSat snowfall retrievals over
ice sheets ?, IEEE Geosciences and remote Sensing Letters 16 (3°,
342-346,
DOI:10.1109/LGRS.2018.2875007
Baas,
P., B. J. H. van de Wiel, E. van Meijgaard , E. Vignon, C.
Genthon, S. J. A. van der Linden, and S. R. de Roode, 2018.
Transitions in the wintertime near-surface temperature inversion
at Dome C, Antarctica, Q. J. R. M. S., doi: 10.1002/qj.3450.
Souverijns,
N., A. Gossart, S. Lhermitte, I. V. Gorodetskaya, J. Grazioli, A.
Berne, C. Durán-Alarcón,
B. Boudevillain, C. Genthon, C. Scarchilli, and N. P. M. van
Lipzig, 2018. Evaluation of the CloudSat surface snowfall product
over Antarctica using ground-based precipitation radars, The
Cryosphere, 12, 3775-3789, 2018, doi.org/10.5194/tc-12-3775-2018.
Durán-Alarcón,
C., B. Boudevillain, C. Genthon, J. Grazioli, N. Souverijns, N. P.
M. van Lipzig, I. Gorodetskaya, et
A.
Berne, 2018. The vertical structure of precipitation at two
stations in East Antarctica derived from micro rain radars,
The
Cryosphere, 3,
247-264, 2019, https://doi.org/10.5194/tc-13-247-2019
Petenko, I., S. Argentini, G. Casasanta, C. Genthon, M. Kallistratova, 2019. Stable Surface-Based Turbulent Layer During the Polar Winter at Dome C, Antarctica: Sodar and In Situ Observations? Bound. Lay. Meteor., 171 – 1, 101–128, https://doi.org/10.1007/s10546-018-0419-6
Lemonnier, F. J-B Madeleine, C. Claud, C.Genthon, C. Durán-Alarcón, C. Palerme, A. Berne, N. Souverijns, N. van Lipzig, I. Gorodetskaya, T. L'Ecuyer, and N. WoodE, 2018. Evaluation of CloudSat snowfall rate profiles by a comparison with in-situ micro rain radars observations in East Antarctica, The Crysophere, in press
And
more publications to be entered soon
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