Niels Weiss

ORCID: 0000-0001-8905-343X
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About
Contact & Profiles
Research Areas
  • Climate change and permafrost
  • Cryospheric studies and observations
  • Geology and Paleoclimatology Research
  • Geological Studies and Exploration
  • Soil and Unsaturated Flow
  • Peatlands and Wetlands Ecology
  • Methane Hydrates and Related Phenomena
  • Atmospheric and Environmental Gas Dynamics
  • Indigenous Studies and Ecology
  • Geotechnical and Geomechanical Engineering
  • Mine drainage and remediation techniques
  • Hydrocarbon exploration and reservoir analysis
  • Arctic and Antarctic ice dynamics
  • Geochemistry and Geologic Mapping
  • Soil and Environmental Studies
  • Smart Materials for Construction
  • Soil Geostatistics and Mapping
  • Heavy metals in environment

Government of Northwest Territories
2022-2023

Wilfrid Laurier University
2023

Stockholm University
2014-2020

University of Amsterdam
2011

Abstract Permafrost‐affected ecosystems are important components in the global carbon (C) cycle that, despite being vulnerable to disturbances under climate change, remain poorly understood. This study investigates ecosystem storage two contrasting continuous permafrost areas of NE and East Siberia. Detailed partitioning soil organic (SOC) phytomass (PC) is analyzed for one tundra (Kytalyk) taiga (Spasskaya Pad/Neleger) area. In total, 57 individual field sites (24 33 respective areas) have...

10.1002/2015jg002999 article EN Journal of Geophysical Research Biogeosciences 2015-09-21

This paper documents the first comprehensive inventory of thermokarst and thaw-sensitive terrain indicators for a 2 million km2 region northwestern Canada. is accomplished through Thermokarst Mapping Collective (TMC), research collaborative to systematically permafrost thaw sensitivity by mapping aerial assessments across Northwest Territories (NT), The increase in NT-based capacity has fostered science leadership collaboration with government, academic, community researchers enable project...

10.1139/as-2023-0009 article EN cc-by Arctic Science 2023-07-17

Abstract. Soils in the northern high latitudes are a key component global carbon cycle; permafrost region covers 22 % of Northern Hemisphere land surface area and holds almost twice as much atmosphere. Permafrost soil organic matter stocks represent an enormous long-term sink which is risk switching to net source future. Detailed knowledge about quantity mechanisms controlling storage utmost importance for our understanding potential impacts feedbacks on climate change. Here we present...

10.5194/essd-14-4095-2022 article EN cc-by Earth system science data 2022-09-07

On January 1st, 2024, the Mw 7.5 Noto Peninsula earthquake ruptured on a series of coastal offshore reverse faults in back arc central Japan. Closest to rupture, northwest, rocks uplifted as much 4.4 m (Fukushima Yo et al., 2024). The coastline accordingly moved seaward by up 200 creating new wide bedrock platforms. Recent Holocene terraces mapped along northern coast (Shishikura 2020), where coseismic uplift was greatest 1st suggest similar past ruptures. Many follow at depth ca. 60 below...

10.5194/egusphere-egu25-11196 preprint EN 2025-03-14

Abstract. The large stocks of soil organic carbon (SOC) in soils and deposits the northern permafrost region are sensitive to global warming thawing. potential release this (C) as greenhouse gases atmosphere does not only depend on total quantity matter (SOM) affected by thawing, but it also depends its lability (i.e., rate at which will decay). In study we develop a simple robust classification scheme SOM for main types region. is based widely available geochemical parameters landscape unit...

10.5194/bg-17-361-2020 article EN cc-by Biogeosciences 2020-01-23

Abstract Decomposition of soil organic matter (SOM) in permafrost terrain and the production greenhouse gases is a key factor for understanding climate change‐carbon feedbacks. Previous studies have shown that SOM decomposition mostly controlled by temperature, moisture, carbon‐nitrogen ratio (C:N). However, focus has generally been on site‐specific processes little known about variations controls across Arctic sites. For assessing decomposition, we retrieved 241 samples from 101 profiles...

10.1002/2017jg004069 article EN Journal of Geophysical Research Biogeosciences 2018-01-24

In this study we assess the total storage, landscape distribution, and vertical partitioning of soil organic carbon (SOC) stocks on Brøgger Peninsula, Svalbard. This type high Arctic area is underrepresented in SOC databases for northern permafrost region. Physico-chemical, elemental, radiocarbon (14C) dating analyses were carried out thirty-two profiles. Results upscaled using both a land cover classification (LCC) landform (LFC). Both LCC LFC approaches provide weighted mean 0–100 cm...

10.1080/15230430.2019.1570784 article EN cc-by Arctic Antarctic and Alpine Research 2019-01-01

Accurate quantity and distribution estimates of permafrost soil organic carbon (SOC) stocks are needed to project potential feedbacks climate, following warming. Still, upscaling from local field observations regional circumarctic assessments remains a challenge. Here we explore elevation-based techniques for High-Arctic SOC stocks. We combine two detailed, high-resolution inventories on Spitsbergen (Svalbard) with validation data. find clear relationship between elevation content, use this...

10.1080/17518369.2017.1400363 article EN cc-by-nc Polar Research 2017-01-01

Abstract. Soils in the northern high latitudes are a key component global carbon cycle; permafrost region covers 22 % of Northern Hemisphere and holds almost twice as much atmosphere. Permafrost soil organic matter stocks represent an enormous long-term sink which is risk switching to net source future. Detailed knowledge about quantity mechanisms controlling storage utmost importance for our understanding potential impacts feedbacks on climate change. Here we present geospatial dataset...

10.5194/essd-2022-8 preprint EN cc-by 2022-02-02

Abstract. The large stocks of soil organic carbon (SOC) in soils and deposits the northern permafrost region are sensitive to global warming thawing. potential release this (C) as greenhouse gases atmosphere does not only depend on total quantity matter (SOM) affected by thawing, but also its lability (i.e. rate at which it will decay). In study we develop a simple robust classification scheme SOM for main types region. is based widely available geochemical parameters landscape unit classes,...

10.5194/bg-2019-89 preprint EN cc-by 2019-05-21
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