Johannes Aschauer

ORCID: 0000-0002-2605-8003
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About
Contact & Profiles
Research Areas
  • Cryospheric studies and observations
  • Climate variability and models
  • Meteorological Phenomena and Simulations
  • Hydrology and Watershed Management Studies
  • Tree-ring climate responses
  • Climate change and permafrost
  • Winter Sports Injuries and Performance
  • Landslides and related hazards
  • Species Distribution and Climate Change
  • Astro and Planetary Science
  • Geology and Paleoclimatology Research
  • Time Series Analysis and Forecasting
  • Planetary Science and Exploration
  • Geotechnical Engineering and Analysis
  • Precipitation Measurement and Analysis

University of Tübingen
2022

Center for Snow and Avalanche Studies
2021-2022

Swiss Federal Institute for Forest, Snow and Landscape Research
2021

University of Freiburg
2017

Abstract Austrian observations of snow depth date back to 1895 and are thus among the longest available quantitative information from hydrometeorological networks worldwide. It is well known that such long‐term prone inhomogeneities, which may not only affect climatologies trends, but derived products used in research or practice. While reliability methods for detecting breaks time series has been shown before could also be confirmed by our work, we focused on improving adjustment method....

10.1002/joc.7742 article EN International Journal of Climatology 2022-05-31

10.1016/j.icarus.2017.02.021 article EN Icarus 2017-03-02

Abstract We investigate relationships between synoptic-scale atmospheric variability and the mass-balance of 13 Andean glaciers (located 16–55° S) using Pearson correlation coefficients (PCCs) multiple regressions. then train empirical glacier models (EGMs) in a cross-validated regression procedure for each glacier. find four distinct glaciological zones with regard to their climatic controls: (1) The Outer Tropics is linked temperature El Niño-Southern Oscillation (PCC ⩽ 0.6), (2) Desert...

10.1017/jog.2022.6 article EN cc-by-nc-nd Journal of Glaciology 2022-02-18

Abstract. Snow cover plays a crucial role in regional climate systems worldwide. It is key variable the context of change because its direct feedback to system, while at same time being very sensitive change. Accurate long-term spatial data on snow are scarce, due lack satellite or forcing run land surface models back time. This study presents an R package, SnowQM, designed correct for bias water equivalent data, using more accurate calibrating correction. The correction based widely applied...

10.5194/gmd-2022-298 preprint EN cc-by 2023-05-17

Abstract. Many methods exist to model snow densification in order calculate the depth of a single layer or total cover from its mass. Most these models need be tightly integrated with an accumulation and melt many forcing variables at high temporal resolution. However, when trying (HS) on climatological timescales, which is often needed for winter tourism-related applications, preconditions can cause barriers. Often, types empirical are used. These estimate snowmelt based daily precipitation...

10.5194/gmd-16-4063-2023 article EN cc-by Geoscientific model development 2023-07-19

Abstract. Knowledge concerning possible inhomogeneities in a data set is of key importance for any subsequent climatological analyses. Well-established relative homogenization methods developed temperature and precipitation exist but have rarely been applied to snow-cover-related time series. We undertook homogeneity assessment Swiss monthly snow depth series by running comparing the results from three well-established semi-automatic break point detection (ACMANT – Adapted Caussinus-Mestre...

10.5194/tc-16-2147-2022 article EN cc-by ˜The œcryosphere 2022-06-09

Abstract. Historic measurements are often temporally incomplete and may contain longer periods of missing data, whereas climatological analyses require continuous measurement records. This is also valid for historic manual snow depth (HS) time series, which even whole winters can be in a station record, suitable methods have to found reconstruct the data. Daily situ HS data from 126 nivo-meteorological stations Switzerland an altitudinal range 230 2536 m above sea level used compare six...

10.5194/gi-10-297-2021 article EN cc-by Geoscientific instrumentation, methods and data systems 2021-11-24

Abstract. Snow plays a crucial role in regional climate systems worldwide. It is key variable the context of change because its direct feedback to system, while at same time being very sensitive change. Long-term spatial data on snow cover and water equivalent are scarce, due lack satellite or forcing run land surface models back time. This study presents an R package, SnowQM, designed correct for bias long-term compared shorter-term more accurate dataset, using calibrate correction. The...

10.5194/gmd-17-8969-2024 article EN cc-by Geoscientific model development 2024-12-19

Abstract. Many methods exist to model snow densification in order calculate the depth of a single layer or total cover from its mass. Most these models need be tightly integrated with an accumulation and melt many forcing variables at high temporal resolution. However, when trying on climatological timescales, which is often needed for winter tourism related applications, preconditions can cause barriers. Often, types applications empirical are used. These estimate based daily precipitation...

10.5194/gmd-2022-258 preprint EN cc-by 2023-01-16

<p>Switzerland has a unique dataset of long-term manual daily snow depth time series ranging back more than 100 years for some stations. This makes the predestined to be analyzed in climatological sense. However, there are sometimes shorter (weeks, months) or longer (years) gaps these series, which hinder sound analysis and reasonable conclusions. Therefore, we examine different methods filling data series. We focus on use spatial interpolation, temperature index models machine...

10.5194/egusphere-egu2020-17211 article EN 2020-03-10

Abstract. Knowledge concerning possible inhomogeneities in a data set is of key importance for any subsequent climatological analyses. Well-established relative homogenization methods developed temperature and precipitation exist, but with only little experience snow. We undertook homogeneity assessment Swiss snow depth series by running comparing the results from three well-established semi-automatic break point detection (ACMANT, Climatol, HOMER). Break points identified each method...

10.5194/tc-2022-48 preprint EN cc-by 2022-03-17

Abstract. Historic measurements are often temporally incomplete and may contain longer periods of missing data whereas climatological analyses require continuous measurement records. This is also valid for historic manual snow depth (HS) time series, where even whole winters can be in a station record suitable methods have to found reconstruct the data. Daily in-situ HS from 126 nivo-meteorological stations Switzerland an altitudinal range 230 2536 m above sea level used compare six...

10.5194/gi-2021-16 preprint EN cc-by 2021-06-09

<p>Models that consume meteorological data have often requirements are quite incompatible with the realities of continuously measured data: they require gapless when datasets gaps, sampling rate matching phenomena interest use a dictated by energy and storage capacities, ‘perfect’ sensors flaws.</p><p> </p><p><span>The MeteoIO library...

10.5194/egusphere-egu2020-19368 article EN 2020-03-10

<p>Measurements of snow depth can vary dramatically over small distances, and as with any other meteorological variable, time series are affected by inhomogeneities or break points. Such arise due to e.g.; changes instrumentation, station location observer practices, in the local environment such urbanisation plant growth.</p><p>In order analyse monitor variation accurately, homogenised data required. In deriving series, it is essential...

10.5194/egusphere-egu22-5379 preprint EN 2022-03-27
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