Results 11 to 20 of about 528 (185)

Greenland bare-ice albedo from PROMICE automatic weather station measurements and Sentinel-3 satellite observations

GEUS Bulletin, 2021
The Programme for Monitoring of the Greenland Ice Sheet (PROMICE) provides surface meteorological and glaciological measurements from widespread on-ice automatic weather stations since mid-2007.
Adrien Wehrlé, Jason E. Box, Masashi Niwano, Alexandre M. Anesio, Robert S. Fausto   +4 more
doaj   +7 more sources

Greenland ice sheet mass balance assessed by PROMICE (1995–2015) [PDF]

Geological Survey of Denmark and Greenland Bulletin, 2019
The Programme for Monitoring of the Greenland Ice Sheet (PROMICE) has measured ice-sheet elevation and thickness via repeat airborne surveys circumscribing the ice sheet at an average elevation of 1708 ± 5 m (Sørensen et al. 2018).
William Colgan, Kenneth D Mankoff, Kristian K Kjeldsen, Anders A Bjørk, Jason E Box, Sebastian B Simonsen, Louise S Sørensen, S. Abbas Khan, Anne M Solgaard, Rene Forsberg, Henriette Skourup, Lars Stenseng, Steen S Kristensen, Sine M Hvidegaard, Michele Citterio, Nanna Karlsson, Xavier Fettweis, Andreas P Ahlstrøm, Signe B Andersen, Dirk van As, Robert S Fausto   +20 more
doaj   +8 more sources

Programme for Monitoring of the Greenland Ice Sheet (PROMICE): first temperature and ablation records [PDF]

Geological Survey of Denmark and Greenland Bulletin, 2011
The Greenland ice sheet is reacting to climate change. Yet, mass-budget estimates differ considerably, partly due to climatic variability and partly to uncertainties in the techniques of assessing mass change (IPCC 2007). Nevertheless, all recent estimates agree that the ice sheet is losing mass (e.g. 286 Gt/yr; Velicogna 2009) at an accelerating rate (
van As, Dirk, Fausto, Robert S, Ahlstrøm, Andreas P, Andersen, Signe B, Andersen, Morten L, Citterio, Michele, Edelvang, Karen, Gravesen, P, Machguth, Horst, Nick, Faezeh M, Nielsen, Søren, weidick, Anker   +11 more
core   +6 more sources

Darkening of the Greenland ice sheet due to the melt albedo feedback observed at PROMICE weather stations [PDF]

Geological Survey of Denmark and Greenland Bulletin, 2013
The Greenland ice sheet is losing mass (Barletta et al. 2012) and at least half of this loss is caused by an increase in surface melt (e.g. Tedesco et al. 2013). The other part is caused by increased dynamic mass loss, as marine-terminating glaciers lose resistive stresses (Nick et al.
van As, Dirk, Fausto, Robert S, Colgan, William T, Box, Jason E, et al   +4 more
core   +5 more sources

PROMICE | GC-NET automatic weather station data [PDF]

Earth System Science Data
We present a new version of the PROMICE | GC-NET automatic weather station (AWS) data product, combining observations from two Greenland AWS networks; PROMICE and GC-NET.
R. S. Fausto, P. How, B. Vandecrux, M. C. Lund, J. E. Box, K. D. Mankoff, K. D. Mankoff, K. D. Mankoff, S. B. Andersen, D. van As, R. Bahbah, M. Citterio, W. Colgan, H. T. Jakobsgaard, N. B. Karlsson, K. K. Kjeldsen, S. H. Larsen, C. Olsen, F. M. Oraschewski, A. Rutishauser, C. L. Shields, A. M. Solgaard, I. T. Stevens, S. H. Svendsen, K. Langley, A. Messerli, A. A. Bjørk, J. K. Andersen, J. Abermann, J. Steiner, R. Prinz, B. Hynek, B. Hynek, B. Hynek, J. M. Lea, S. Brough, A. P. Ahlstrøm   +36 more
doaj   +3 more sources

Circum-Greenland, ice-thickness measurements collected during PROMICE airborne surveys in 2007, 2011 and 2015 [PDF]

Geological Survey of Denmark and Greenland Bulletin, 2018
The Greenland ice sheet has experienced an average mass loss of 142 ± 49 Gt/yr from 1992 to 2011 (Shepherd et al. 2012), making it a significant contributor to sea-level rise. Part of the ice- sheet mass loss is the result of increased dynamic response of outlet glaciers (Rignot et al. 2011).
Louise Sandberg Sørensen, Sebastian B. Simonsen, René Forsberg, Lars Stenseng, Henriette Skourup, Steen Savstrup Kristensen, William Colgan   +6 more
core   +4 more sources

Review of Survey activities 2010: Programme for Monitoring of the Greenland Ice Sheet (PROMICE): first temperature and ablation records [PDF]

Geological Survey of Denmark and Greenland Bulletin, 2011
As, Dirk van, Fausto, Robert S., PROMICE project team   +2 more
doaj   +2 more sources

Review of Survey activities 2011: Ablation observations for 2008–2011 from the Programme for Monitoring of the Greenland Ice Sheet (PROMICE) [PDF]

Geological Survey of Denmark and Greenland Bulletin, 2012
Fausto, R.S., van As, D., PROMICE project team   +2 more
doaj   +2 more sources

Targeting dipeptidyl peptidase 3 (DPP3) in extreme-critically ill patients with refractory shock: First-in-human report on the safety and efficacy of an anti-DPP3 antibody. [PDF]

Eur J Heart Fail
European Journal of Heart Failure, Volume 27, Issue 8, Page 1483-1485, August 2025.
Jarczak D, Nierhaus A, Mebazaa A, Herpain A, Pickkers P, Anar S, Kluge S.   +6 more
europepmc   +2 more sources

Haemodynamic effects of istaroxime in SCAI stage B HF-related cardiogenic shock: Insights from the SEISMiC trial. [PDF]

ESC Heart Fail
Among patients with ADHF‐related SCAI stage B CS enrolled in SEISMiC, istaroxime at doses up to 1.0 μg/kg/min for up to 60 h was associated with sustained improvements in aortic pulsatility index and LV stroke work index, and with increase of PA compliance and reduction in PA elastance at 48 h.
Pagnesi M, Cotter G, Davison B, Burkhoff D, Mebazaa A, Biegus J, Chioncel O, Edwards C, Takagi K, Filippatos G, Tycińska A, Novosadova M, Gulati G, Barros M, Diaz ML, Guardia C, Zymliński R, Gajewski P, Ponikowski P, Simmons P, Simonson S, Metra M.   +21 more
europepmc   +2 more sources