A. J. Dolman

ORCID: 0000-0003-0099-0457
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About
Contact & Profiles
Research Areas
  • Atmospheric and Environmental Gas Dynamics
  • Plant Water Relations and Carbon Dynamics
  • Climate variability and models
  • Climate change and permafrost
  • Meteorological Phenomena and Simulations
  • Peatlands and Wetlands Ecology
  • Cryospheric studies and observations
  • Atmospheric chemistry and aerosols
  • Hydrology and Watershed Management Studies
  • Methane Hydrates and Related Phenomena
  • Soil Moisture and Remote Sensing
  • Forest ecology and management
  • Fire effects on ecosystems
  • Tree-ring climate responses
  • Geology and Paleoclimatology Research
  • Climate Change Policy and Economics
  • Atmospheric Ozone and Climate
  • Soil Carbon and Nitrogen Dynamics
  • Plant responses to elevated CO2
  • Precipitation Measurement and Analysis
  • Remote Sensing in Agriculture
  • Plant Ecology and Soil Science
  • Environmental Impact and Sustainability
  • Soil and Unsaturated Flow
  • Hydrocarbon exploration and reservoir analysis

Vrije Universiteit Amsterdam
2015-2025

Royal Netherlands Institute for Sea Research
2020-2025

Netherlands Earth System Science Centre
2022-2023

Utrecht University
1955-2023

Nederlands Instituut Voor Zuivel Oonderzoek
2022

Finnish Meteorological Institute
2021

Chinese University of Hong Kong
2021

Northern Arizona University
2021

University of Helsinki
2021

University of Alaska Fairbanks
2021

Abstract. This paper outlines a new strategy to derive evaporation from satellite observations. The approach uses variety of satellite-sensor products estimate daily at global scale and 0.25 degree spatial resolution. Central this methodology is the use Priestley Taylor (PT) model. minimalistic PT equation combines small number inputs, majority which can be detected space. reduces variables that need modelled. Key distinguishing features are microwave-derived soil moisture, land surface...

10.5194/hess-15-453-2011 article EN cc-by Hydrology and earth system sciences 2011-02-03
Gilberto Pastorello Carlo Trotta Eleonora Canfora Housen Chu Danielle Christianson and 95 more You-Wei Cheah C. Poindexter Jiquan Chen Abdelrahman Elbashandy Marty Humphrey Peter Isaac Diego Polidori Markus Reichstein Alessio Ribeca Catharine van Ingen Nicolas Vuichard Leiming Zhang B. D. Amiro Christof Ammann M. Altaf Arain Jonas Ardö Timothy J. Arkebauer Stefan K. Arndt Nicola Arriga Marc Aubinet Mika Aurela Dennis Baldocchi Alan Barr Eric Beamesderfer Luca Belelli Marchesini Onil Bergeron Jason Beringer Christian Bernhofer Daniel Berveiller D. P. Billesbach T. Andrew Black Peter D. Blanken Gil Bohrer Julia Boike Paul V. Bolstad Damien Bonal Jean-Marc Bonnefond D. R. Bowling Rosvel Bracho Jason Brodeur Christian Brümmer Nina Buchmann Benoît Burban Sean P. Burns Pauline Buysse Peter Cale M. Cavagna Pierre Cellier Shiping Chen Isaac Chini Torben R. Christensen James Cleverly Alessio Collalti Claudia Consalvo Bruce D. Cook David Cook Carole Coursolle Edoardo Cremonese Peter S. Curtis Ettore D’Andrea Humberto da Rocha Xiaoqin Dai K. J. Davis Bruno De Cinti A. de Grandcourt Anne De Ligne Raimundo Cosme de Oliveira Nicolas Delpierre Ankur R. Desai Carlos Marcelo Di Bella Paul Di Tommasi A. J. Dolman Francisco Domingo Gang Dong Sabina Dore Pierpaolo Duce Éric Dufrêne Allison L. Dunn Jiří Dušek Derek Eamus Uwe Eichelmann Hatim Abdalla M. ElKhidir Werner Eugster Cäcilia Ewenz B. E. Ewers D. Famulari Silvano Fares Iris Feigenwinter Andrew Feitz Rasmus Fensholt Gianluca Filippa M. L. Fischer J. M. Frank Marta Galvagno Mana Gharun

Abstract The FLUXNET2015 dataset provides ecosystem-scale data on CO 2 , water, and energy exchange between the biosphere atmosphere, other meteorological biological measurements, from 212 sites around globe (over 1500 site-years, up to including year 2014). These sites, independently managed operated, voluntarily contributed their create global datasets. Data were quality controlled processed using uniform methods, improve consistency intercomparability across sites. is already being used...

10.1038/s41597-020-0534-3 article EN cc-by Scientific Data 2020-07-09

Summary This paper presents CO 2 flux data from 18 forest ecosystems, studied in the European Union funded EUROFLUX project. Overall, mean annual gross primary productivity (GPP, total amount of carbon (C) fixed during photosynthesis) these forests was 1380 ± 330 gC m −2 y −1 (mean ±SD). On average, 80% GPP respired by autotrophs and heterotrophs released back into atmosphere (total ecosystem respiration, TER = 1100 260 ). Mean soil respiration (SR) 760 340 (55% 69% TER). Among investigated...

10.1046/j.1365-2486.2001.00412.x article EN Global Change Biology 2001-03-01

Abstract Terrestrial ecosystems sequester 2.1 Pg of atmospheric carbon annually. A large amount the terrestrial sink is realized by forests. However, considerable uncertainties remain regarding fate this over both short and long timescales. Relevant data to address these are being collected at many sites around world, but syntheses still sparse. To facilitate future synthesis activities, we have assembled a comprehensive global database for forest ecosystems, which includes budget variables...

10.1111/j.1365-2486.2007.01439.x article EN Global Change Biology 2007-08-21

Most inverse atmospheric models report considerable uptake of carbon dioxide in Europe's terrestrial biosphere. In contrast, stocks ecosystems increase at a much smaller rate, with gains forests and grassland soils almost being offset by losses from cropland peat soils. Accounting for non-carbon transfers that are not detected the fluxes bypassing ecosystem considerably reduces gap between small carbon-stock changes larger estimated models. The remaining difference could be because missing...

10.1126/science.1083592 article EN Science 2003-05-22

Abstract Methane (CH 4 ) is produced in many natural systems that are vulnerable to change under a warming climate, yet current CH budgets, as well future shifts emissions, have high uncertainties. Climate has the potential increase emissions from critical such wetlands, marine and freshwater systems, permafrost, methane hydrates, through temperature, hydrology, vegetation, landscape disturbance, sea level rise. Increased these would turn induce further climate change, resulting positive...

10.1002/2017rg000559 article EN cc-by-nc-nd Reviews of Geophysics 2018-02-16

Abstract This paper overviews the short‐term (biophysical) and long‐term (out to around 100 year timescales; biogeochemical biogeographical) influences of land surface on weather climate. From our review literature, evidence is convincing that terrestrial ecosystem dynamics these timescales significantly influence atmospheric processes. In studies past possible future climate change, are as important changes in composition, ocean circulation, ice sheet extent, orbit perturbations.

10.1046/j.1365-2486.1998.t01-1-00176.x article EN Global Change Biology 1998-06-01

This paper overviews the short-term (biophysical) and long-term (out to around 100 year timescales; biogeochemical biogeographical) influences of land surface on weather climate. From our review literature, evidence is convincing that terrestrial ecosystem dynamics these timescales significantly influence atmospheric processes. In studies past possible future climate change, are as important changes in composition, ocean circulation, ice sheet extent, orbit perturbations.

10.1046/j.1365-2486.1998.00176.x article EN Global Change Biology 1998-06-01

Abstract. A process-based methodology is applied to estimate land-surface evaporation from multi-satellite information. GLEAM (Global Land-surface Evaporation: the Amsterdam Methodology) combines a wide range of remotely-sensed observations derive daily actual and its different components. Soil water stress conditions are defined root-zone profile soil moisture used transpiration based on Priestley Taylor equation. The also derives evaporationfrom bare snow sublimation. Tall vegetation...

10.5194/hess-15-967-2011 article EN cc-by Hydrology and earth system sciences 2011-03-17

Drainage of peatlands and deforestation have led to large-scale fires in equatorial Asia, affecting regional air quality global concentrations greenhouse gases. Here we used several sources satellite data with biogeochemical atmospheric modeling better understand constrain fire emissions from Indonesia, Malaysia, Papua New Guinea during 2000-2006. We found that average this region [128 +/- 51 (1sigma) Tg carbon (C) year(-1), T = 10(12)] were comparable fossil fuel emissions. In Borneo,...

10.1073/pnas.0803375105 article EN Proceedings of the National Academy of Sciences 2008-12-16

Abstract. Land evapotranspiration (ET) estimates are available from several global data sets. Here, monthly land ET synthesis products, merged these individual sets over the time periods 1989–1995 (7 yr) and 1989–2005 (17 yr), presented. The products shorter period based on a total of 40 distinct while those longer 14 In sets, is derived satellite and/or in situ observations (diagnostic sets) or calculated via land-surface models (LSMs) driven with observations-based forcing output...

10.5194/hess-17-3707-2013 article EN cc-by Hydrology and earth system sciences 2013-10-01

Within the scope of upcoming launch a new water related satellite mission (SMOS) global evaluation study was performed on two available soil moisture products. ERS scatterometer surface wetness data compared to AMSR-E data. This pointed out strong similarity between both products in sparse moderate vegetated regions with an average correlation coefficient 0.83. Low correlations were found densely areas and deserts. The low values can be explained by limited retrieval capabilities over dense...

10.1007/s10712-008-9044-0 article EN cc-by-nc Surveys in Geophysics 2008-10-01

Abstract. The WAter Cycle Multi-mission Observation Strategy – EvapoTranspiration (WACMOS-ET) project aims to advance the development of land evaporation estimates on global and regional scales. Its main objective is derivation, validation, intercomparison a group existing retrieval algorithms driven by common forcing data set. Three commonly used process-based methodologies are evaluated: Penman–Monteith algorithm behind official Moderate Resolution Imaging Spectroradiometer (MODIS) product...

10.5194/hess-20-823-2016 article EN cc-by Hydrology and earth system sciences 2016-02-23

An alternative to thermal infrared satellite sensors for measuring land surface temperature ( T s ) is presented. The 37 GHz vertical polarized brightness used derive because it considered the most appropriate microwave frequency retrieval. This channel balances a reduced sensitivity soil characteristics with relatively high atmospheric transmissivity. It shown that simple linear relationship, accurate values can be obtained from this frequency, theoretical bias of within 1 K 70% vegetated...

10.1029/2008jd010257 article EN Journal of Geophysical Research Atmospheres 2009-02-24
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