CENPERM activities Per Ambus, Anders Michelsen, Laura Helene Rasmussen, Laura Bjørnholt Larsen, Emily Pickering Pedersen, Ludovica D'Imperio, Andreas Westergaard-Nielsen, Trevor James Popp, Steffen Bo Hansen, Sune Olander Rasmussen, Bo Elberling, University of Copenhagen, Denmark, Peter Convey, British Antarctic Survey, United Kingdom Ice core project Ice cores were collected in April 2018 from both Lyngmarksbræen and Storbræen and 1710 samples have subsequently been analysed for dD, d18O, and deuterium excess at 2.5 cm resolution. For isotopes, Lyngmarksbræen is complete (ca. 17.3 m/660 samples at 2.5 cm) and Storbræen is complete to about 26.4 m/1050 samples at 2.5 cm. The aim is to quantify seasonal air temperature trends within the last 200 years and compare these with cores from the Greenland Ice Sheet and with dendrochronology based dates on vegetation growth at Disko. Snow model Repeated drone flying in Blæsedalen was completed in April 2018. The snow distribution in spring 2018 was quantified by comparing these images with drone images from the summer of 2017. Snow cores were taken along transects to provide a proxy for landscape distribution of snow water equivalent. Leaves and permafrost cores Combined samples of permafrost and leaves were collected along a transect from the south-facing slope north of the Moraine lake slope as part of a 15N-labelling experiment. Here, nitrogen was added at the permafrost table and the plant uptake was quantified down-slope. Nitrous oxide emissions from contrasting tundra soils A field study to investigate nitrous oxide (N 2 O) emissions from a dry and a wet tundra ecosystem manipulated in terms of increased air temperature and winter snow cover. Data has been collected in the Snowfence experiment in 2015, 2016 and 2018. Preliminary results from 2015 and 2016 show that the tundra is a source to N 2 O transiently enhanced by increased winter snow. The wet tundra is a stronger source to N 2 O compared to dry tundra. Tundra fire A field study was executed in order to investigate the short- and long-term impacts of Arctic wildfires on tundra ecosystem functions and characteristics. We deployed a controlled tundra fire in 2017, and measured greenhouse gas fluxes and soil geochemical cycles immediately after the fire in 2017 and again during the 2018 growing season. The work continues in 2019. 20 The initial observations reveal that fire exposed tundra has enhanced loss of CO 2 and increased soil nitrogen concentrations. Controlled tundra fre. Photo: Per Ambus. Diversity and life histor y changes in inver tebrate communities under snow and burning manipulations Soil samples were taken in plots manipulated with stable N-isotopes to examine nitrogen flows through the terrestrial food web. Invertebrates were extracted at the station and are now being analysed. Soil nitrogen dynamics along a snow-bed gradient A field study addresses the temporal and spatial variation in soil nitrogen turnover and transport along a natural inclination with contrasting snow cover and snow melt. The work includes in-situ tracing of stable isotopes to reveal internal transport and turnover processes. Observations on greenhouse gas fluxes are also included. The work was initiated in 2018 and continues in 2019. Root scanning The presence of roots have been quantified using minirhizotrons since snow fences were installed in 2013. High-resolution measurements were made during 2018 at both snow fences in the heath (Dry) and in the fen (Wet). Results from previous growing seasons show that root growth can continue until mid-September and plots from wet tundra exposed to experimental warming show a significant increase in root numbers and length but a significant reduction in root diameter in plots with increased snow accumulation. Inspecting camera set-up in Blæsedalen. Photo: Charlotte Sigsgaard. university of copenhagen facu lt y of sci e nc e A RC T I C STAT I ON Ann ual Repor t 2 018 2 A R C T I C S TAT I O N ARCTIC STATION Annual Report 2018 CONTENTS Chairmans welcome ............................................................ 5 Monitoring at Arctic Station ........ .......................................... 6 Research projects ........................ ......................................... 17 Educa 4 Chairmans Welcome Professor Bo Elberling Compared to other years, the summer of 2018 was cold and wet in Greenland. While summer temperatures in Europe were higher than for decades, summer temperatures at Arctic Station were in general low. Despite the weather, the year 2018 has been a very succes Monitoring at Arctic Station Charlotte Sigsgaard, Regin Rønn, Michele Citterio, Jakob Abermann, Per Juel Hansen, Kirsty Langly, Kirsten S. Christoffersen, Sille Myreng, Daniel Binder, Laura Helene Rasmussen, Morten Rasch, Aart Kroon, Dorthe Krause-Jensen, Birgit Olesen, Thomas Friborg and Bo Elberli 15 10 10 Temperature (oC) Temperature (oC) 5 0 -5 -10 -15 Summer (J, J, A) Winter/coldest months (J, F, M) Mean annual air temperature -20 -25 1992 1996 2000 2004 2008 2012 2016 Figure 2. Annual mean air temperatures at Arctic Station from 1992 to 2018 and mean air temperatures for 31-J an 2-Mar 1-Apr 1-May 31-May 30-J un 30-J ul 29-Aug 28-S ep 28-Oct 27-Nov 27-Dec 2018 1040 1000 960 60 0 40 -10 20 -30 0 Wind speed (m s -1) -20 Rain (mm) 80 10 Temperature (C) Air pressure (mbar) 1-J an 16 12 8 4 0 Wind dir () 300 200 100 S now depth (m) 0 0.8 40 0 Sep Precipitation (mm) 350 Aug Jul Jun May 30 0 250 20 0 150 10 0 50 19 91 19 92 19 93 19 94 19 95 19 96 19 97 19 98 19 99 20 00 20 01 20 02 20 03 20 04 20 05 20 06 20 07 20 08 20 09 20 10 20 11 20 12 20 13 20 14 20 15 20 16 20 17 20 18 0 Figure 5. Stacked monthly values of rain from Figure 7. Water started to run in the snow covered river bed on 6 June. Several fows with a mixture of water, snow and ice occurred during the day. Photos: Charlotte Sigsgaard and Laura L. Frendrup. Marine monitoring Marine monitoring has been periodically carried out at Arc tic Station since 1924. Figure 9. About 60-70 mm of rain on the 3 August 2018 caused overland fow and high discharge and high content of suspended sediment in the river. Photo: Elisabeth L. Kolstad. there is of ten a layer of cold water at 50 -10 0 m with temperatures as low as -1.6 C sandwiched bet ween the warmer sur fa Macroalgae monitoring 8 7 10 m 50 m 200 m The Greenland Ecosystem Monitoring program (GEM) on marine vegetation in the Disko Bay was initiated in the summer of 2018. The program includes studies of tidal and subtidal macroalgae along the shores of Disko Island and Kronprinsens Ejland as specified Figure 13. Overview, based on drone images, of Fortuna Bay with the tidal vegetation forming a fringe along the shoreline visible as a light brown contour at low tide. Drone operated by Dorte KrauseJensen and Birgit Olesen and drone images analysed and processed by Michael Bo Rasmussen. Growth of s 14 Chlorophyll (ug l-1) 12 Danish Meteorological Institute (DM I) which will pro vide data for in-situ validation data for DM Is remote sensing produc t s. The first complete dataset will be downloaded in 2019. Data received via satellite link already shows seasonal variabilit y in the temperatur Figure 18. Two moulins on Chamberlin Glacier found in August 2018 (left) and the entrance of one of the moulins which in August 2018 appeared safe to descend. Photos: Michele Citterio. Influence of cloud cover in surface energy balance in Arctic environments Sur face air temperatures in the Arctic enhance snow and glacier melt is still poorly known, not the least in Greenland. While some authors claim clouds enhance melt water runof f others claim that decreasing cloud cover drives the recent mass loss on the Greenland ice sheet. Despite their crucial impor tance for understanding Arc tic cli Research Projects Development of methodology for evaluating chemicals discarded in high Arctic waters Kim Gustavson, Eva Friis Møller, Mette Dalgaard, DCE, Department of Bioscience Aarhus University, Denmark The overall aim of the project was to strengthen the basis for evaluation and regulation of Baleen whale. Photo: Mads Peter Heide-Jørgensen. Qimmeq Anders J. Hansen, Tom Gilbert, University of Copenhagen, Denmark, Nobuyuki Yamaguchi, Qatar University, Quatar, Siz Madsen, Denmark The Qimmeq Project consists of several components including, sled dog genetics, culture history, film- and phot Greenlandic Perspectives Survey (GPS) AMAP - collection of ring seal samples Kelton Minor, University of Copenhagen, Kraks Fond Institute for Urban Economic Research, Denmark, Ulunnguaq Markussen, University of Greenland, Greenland, Hans Peter Mønsted, University of Southern Denmark, Denmark Sign CENPERM activities Per Ambus, Anders Michelsen, Laura Helene Rasmussen, Laura Bjørnholt Larsen, Emily Pickering Pedersen, Ludovica D'Imperio, Andreas Westergaard-Nielsen, Trevor James Popp, Steffen Bo Hansen, Sune Olander Rasmussen, Bo Elberling, University of Copenhagen, Denmark, Peter Convey, Brit A n n u a l R e p o r t 2018 21 Preparing samples in the laboratory . Photo: Advanced Analytical Chemistry - Arctic Pollution Chemistry 2018 (Field course) Photo Kent Pørksen 22 Education CHESS PhD school: Arctic Glacier Field Course Alexios Theofilopoulos, Andreas Alexander, Anais Bretones, Andreas Plach, Calvin Shackleton, Ida Margrete Ringgaard, Jacob Morgan, Jonathan Rheinlander, Karita Kajanto, Lis Allaar t, Margaret Lindeman, Maya Becker, Mor ven Muilwijk, Nicholas Ra Field trip North Greenlands High School GUX Asiaat Photo: Advanced Analytical Chemistry -Arctic Pollution Research 2018 (Field course). All projec ts included numerous sampling trips in the field (open water and coast line) followed by analyses in dif ferent designated labs at the Arc tic Station based monitoring projec t focusing on the conditions of the living resources based on input from local fishers and hunters. Visiting period: 5 December, 2 days. Climate Change in Greenland Niels Vinther, Egedal Gymnasium, A sger Vinther Michelsen, Kenneth Sorento, Mediehuset København Denmark Visit Publications Scientific papers 2018 A lb e r s C. N ., K ra m s h ø j M ., R inna n R . (2018). R a p i d min e ra liz at i o n of b i o g e ni c vo lat il e o rg a ni c co m p o un d s in te m p e rate a n d A rc t i c s o ils . B i o g e o s ci e n ce s 15, 3591-3 6 01. D O I :10.519 4 / b g -15 - Reports 2018 K a li t a, S . N ., Wo hlra b, S ., Ku e hn e, N . a n d J o hn, U., A l fre d - We g e n e r- I ns t i tu te (2018): Tra ns c r ipto m e ana l y s is of sing l e ce lls: a p la nk to n cha ra c te r iz at i o n of A rc t i c wate r s , 2n d A nnua l M e e t ing of D F G -S P P 19 91 T Members of the board Professor Anders Michelsen Depar tment of Biology Phone: + 45 2339 8286 E-mail: andersm@bio.ku.dk Professor Bo Elberling (Chairman) Depar tment of Geosciences and Natural Resource Management Phone: + 45 3532 2520 E-mail: be@ign.ku.dk A ssociate Professor Nina Lundholm Natural A n n u a l R e p o r t 2018 29 Title Arc tic Station Annual Repor t 2018 Publisher Board of the Arc tic Station, Univer sit y of Copenhagen, Denmark Editor A ar t Kroon and Charlot te Sigsgaard L ayout and graphic s Kent Pørk sen, Depar tment of Geosciences and Natural Resource Management Internet ver sion ark tisk station.ku.dk