Waldemar Walczowski

ORCID: 0000-0002-0243-3307
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About
Contact & Profiles
Research Areas
  • Arctic and Antarctic ice dynamics
  • Oceanographic and Atmospheric Processes
  • Methane Hydrates and Related Phenomena
  • Climate change and permafrost
  • Cryospheric studies and observations
  • Marine and environmental studies
  • Geological Studies and Exploration
  • Atmospheric and Environmental Gas Dynamics
  • Marine and coastal ecosystems
  • Climate variability and models
  • Marine and fisheries research
  • Maritime Navigation and Safety
  • Maritime Transport Emissions and Efficiency
  • Ocean Acidification Effects and Responses
  • Arctic and Russian Policy Studies
  • Geophysics and Gravity Measurements
  • Atmospheric chemistry and aerosols
  • Scientific Research and Discoveries
  • Geology and Paleoclimatology Research
  • Food Industry and Aquatic Biology
  • Winter Sports Injuries and Performance
  • Cruise Tourism Development and Management
  • Marine Biology and Ecology Research
  • Tropical and Extratropical Cyclones Research
  • Isotope Analysis in Ecology

Instytut Oceanologii Polskiej Akademii Nauk
2012-2024

Polish Academy of Sciences
2013-2024

Polish Academy of Learning
2015

United States Navy
2003

United States Department of the Navy
2003

Naval Postgraduate School
2001

The Argo Program has been implemented and sustained for almost two decades, as a global array of about 4000 profiling floats. provides continuous observations ocean temperature salinity versus pressure, from the sea surface to 2000 dbar. successful installation its innovative data management system arose opportunistically combination great scientific need technological innovation. Through system, fundamental physical with broad societally-valuable applications, built on cost-efficient robust...

10.3389/fmars.2019.00439 article EN cc-by Frontiers in Marine Science 2019-08-02

Hydrographic time series in the northeast North Atlantic and Nordic Seas show that freshening trend of 1960s–1990s has completely reversed upper ocean. Since 1990s temperature salinity have rapidly increased Inflow from eastern subpolar gyre to Fram Strait. In 2003–2006 values reached previous maximum last observed around 1960, exceeded records. The mean properties decrease northwards, but variations seen at 57°N persist with same amplitude pattern along pathways Time correlations extreme...

10.1029/2007gl032675 article EN Geophysical Research Letters 2008-02-01

The northward flow of Atlantic Water via the Barents Sea and Fram Strait is modeled, climatological volume, heat, salt fluxes into Arctic Ocean are investigated. We argue that understanding climate change in region requires knowledge mean circulation before its variability can be determined. Since estimates long‐term not available from observations, we present a modeling approach to quantify transports Norwegian Ocean. A coupled ice‐ocean model pan‐Arctic configured at 1/12° 45‐level grid...

10.1029/2001jc001039 article EN Journal of Geophysical Research Atmospheres 2004-03-01

Abstract Oceanographic observations of the Nordic Seas show significant interannual variability inflowing Atlantic Water properties and currents structure. Variations oceanic heat advected northward with influence climate. The aim study was examination, how changes West Spitsbergen Current pathways local climate conditions in Fram Strait region. Results from carried by Institute Oceanology Polish Academy Sciences summers 2000–2007 were compared time series air temperature sea ice north...

10.1002/joc.2338 article EN International Journal of Climatology 2011-04-21

A recent study has shown increased warming in the fjords of west Spitsbergen. Their location is critical, as they are situated along main northward pathway Atlantic Water (AW) which a great source heat to Arctic Ocean and fjords. In light ongoing warming, we aim discuss differences between under transformation oceanic waters. We compared summer hydrographic conditions two located opposite ends Spistbergen: Hornsund south Kongsfjorden north. The based on high resolution CTD measurements...

10.1016/j.oceano.2017.07.003 article EN cc-by-nc-nd Oceanologia 2017-07-26

Abstract We present measurements from two shipboard surveys conducted in summer 2012 that sampled the rim current system around Nordic Seas Fram Strait to Denmark Strait. The data reveal that, along a portion of western boundary Seas, East Greenland Current (EGC) has three distinct components. In addition well‐known shelfbreak branch, there is an inshore branch on continental shelf as well separate offshore shelfbreak. inner contributes significantly overall freshwater transport system, and...

10.1002/2016jc012228 article EN publisher-specific-oa Journal of Geophysical Research Oceans 2017-02-15

Glaciers draining to the Hornsund basin (southern Spitsbergen, Svalbard) have experienced a significant retreat and mass volume loss over last decades, increasing input of freshwater into fjord. An increase in can influence fjord hydrology, hydrodynamics, sediment flux biota, especially changing climate. Here, we describe sources supply based on glaciological meteorological data from period 2006 2015. The average land bay is calculated as 2517 ± 82 Mt a−1, with main contributions glacier...

10.33265/polar.v38.3506 article EN cc-by-nc Polar Research 2019-04-16

Progressive warming of the West Spitsbergen Current (WSC) has been observed since 2004. During summer 2006 temperature and salinity core Atlantic Water (AW) reached highest ever by Institute Oceanology Polish Academy Sciences (IOPAS) values. The structure WSC, heat content extent AW in Fram Strait (FS) region also changed. Temperature changes resulted from upstream Norwegian‐Atlantic (NwAC); WSC its were modified northward advection large mesoscale eddies within western branch 2005. These...

10.1029/2007gl029974 article EN Geophysical Research Letters 2007-05-01

The dramatic changes in the Arctic climate observed recent years have generated an urgent need to investigate Ocean's heat budget. Mooring data and synoptic observations Fram Strait (FS) region shown that increasing amounts of been transported into Ocean (AO) times. Here we present results from conducted West Spitsbergen Current (WSC) summers 2000–2005. study was motivated by strong warm anomalies seen Atlantic Water (AW) layer over a large area WSC, WSC structure. We conclude signal only...

10.1029/2006gl025872 article EN Geophysical Research Letters 2006-06-01

Abstract Walczowski, W., Piechura, J., Goszczko, I., and Wieczorek, P. 2012. Changes in Atlantic water properties: an important factor the European Arctic marine climate. – ICES Journal of Marine Science, 69: 864–869. The advection warm (AW) through Nordic Seas its transformation (cooling freshening) is one most climatological processes region. Time-series hydrographic observations northern Fram Strait region are presented analysed. Significant variability properties AW has been observed...

10.1093/icesjms/fss068 article EN ICES Journal of Marine Science 2012-05-03

Abstract Kwasniewski, S., Gluchowska, M., Walkusz, W., Karnovsky, N. J., Jakubas, D., Wojczulanis-Jakubas, K., Harding, A. M. A., Goszczko, I., Cisek, Beszczynska-Möller, Walczowski, Weslawski, J. and Stempniewicz, L. 2012. Interannual changes in zooplankton on the West Spitsbergen Shelf relation to hydrography their consequences for diet of planktivorous seabirds. – ICES Journal Marine Science, 69: 890–901. The purpose work was determine how atmospheric oceanic processes (the North Atlantic...

10.1093/icesjms/fss076 article EN ICES Journal of Marine Science 2012-05-18

Abstract. The structures of the hydrographic fronts separating Atlantic-origin waters from ambient in northern Nordic Seas are discussed. Flows western and eastern branches West Spitsbergen Current create Atlantic domain borders maintain these fronts. This work is based on previous research investigations carried out project DAMOCLES (Developing Arctic Modelling Observational Capabilities for Long-term Environmental Studies). Most observational data were collected during R/V Oceania cruises....

10.5194/os-9-957-2013 article EN cc-by Ocean science 2013-11-14

Progressing warming in the Arctic and increased extreme weather events can significantly influence hydrography of Svalbard fjords, leading to changes towards more Atlantic-type waters fjords. In this paper, we look into hydrographic conditions Hornsund, southernmost fjord on west coast Svalbard, by analysing high-resolution CTD measurements collected July during cruises with RV Oceania between 2001 2015. These observations revealed high interannual variability temperature, salinity...

10.1080/17518369.2018.1495546 article EN cc-by-nc Polar Research 2018-01-01

Abstract Many Arctic marine‐terminating glaciers have undergone rapid retreats in recent decades. Seasonal and year‐to‐year variations terminus position act on all tidewater glaciers, but the key controls those changes vary from region to region. Here, we examined seasonal decadal termini positions of seven inner part Hornsund, southernmost fjord Spitsbergen (Svalbard Archipelago), based a variety data 1992 2020. Combining satellite imagery, basic meteorological (air temperature, positive...

10.1029/2022jf006911 article EN Journal of Geophysical Research Earth Surface 2023-05-01

Since 1987 annual summer cruises to the Nordic Seas and Fram Strait have been conducted by IO PAN research vessel Oceania under long-term monitoring program AREX. Here we present a short description of measurements preliminary results obtained during open ocean part AREX 2016 cruise. Spatial distributions Atlantic water temperature salinity in are similar their mean fields except for warmer recirculation northern Strait. The longest observation record from section N along 76°30′N reveals...

10.1016/j.oceano.2016.12.003 article EN cc-by-nc-nd Oceanologia 2017-01-13

Abstract Glacierised coasts undergo faster geomorphic processes than unglaciated ones. We have studied changes of the coastal area in southern Svalbard with glacier bridge between Torell Land and Sørkapp since beginning 20th century. The existence a continuous subglacial depression beneath Hornbreen–Hambergbreen system has been debated 1960s, inconclusive results. In this study we assess both topography bathymetry Hornsund Fjord Hambergbukta bay. This included ~40 km radar surveys over...

10.1002/esp.4251 article EN Earth Surface Processes and Landforms 2017-09-07

Abstract Recent observations confirm the rising temperatures of Atlantic waters transported into Arctic Ocean via West Spitsbergen Current ( WSC ). We studied overall abundance and population structure North keystone zooplankton copepod Calanus finmarchicus , which is main prey for pelagic fish some seabirds, in relation to selected environmental variables this area between 2001 2011, when warming Subarctic was particularly pronounced. Sampling within a 3‐week time window each summer...

10.1111/gcb.13864 article EN Global Change Biology 2017-08-12

Abstract The mechanism of glacier recession and its climatic controls are complex processes that differ across the Arctic region. Here, we investigate factors influencing front variations Hansbreen, a terminated in Hornsund fjord (SW Svalbard). We apply remote sensing data to observe fluctuations between 1992 2015 compare them atmospheric oceanographic data, sea water depth at terminus surface velocity. Rate subglacial meltwater discharge approximated by seasonal positive degree‐day index...

10.1029/2020jf005763 article EN Journal of Geophysical Research Earth Surface 2020-12-11

The ocean plays a key role in the climate system, and therefore change threat. About 90% of heat excess absorbed since 1970’s is stored changes hydrological cycle related to are also strongly manifested ocean. In addition, acts as net anthropogenic carbon sink, presently assessed one fourth global uptake, moderator change. It paramount importance monitor properties over long periods, with coverage.Argo has transformed way observing last decades most important source situ marine...

10.5194/egusphere-egu25-19623 preprint EN 2025-03-15
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