Relevance of near-surface soil moisture vs. terrestrial water storage for global vegetation functioning

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Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource, 15 Seiten

Language: Englisch

Bibliographic citation: In: Biogeosciences(21), H. 6, S.1533-1547 - ISSN 1726-4189
In: Copyright: © 2024 Prajwal Khanal et al., Katlenburg-Lindau

Event: Veröffentlichung

(where): Jena

(who): Friedrich-Schiller-Universität Jena

(when): 2024

Creator: Khanal, Prajwal
Hoek Van Dijke, Anne J.
Schaffhauser, Timo
Li, Wantong
Paulus, Sinikka J.
Zhan, Chunhui
Orth, René

URN: urn:nbn:de:gbv:27-dbt-60807-7

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 14.08.2025, 10:59 AM CEST

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Associated

Khanal, Prajwal
Hoek Van Dijke, Anne J.
Schaffhauser, Timo
Li, Wantong
Paulus, Sinikka J.
Zhan, Chunhui
Orth, René
Friedrich-Schiller-Universität Jena

Time of origin

2024

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Network motifs shape distinct functioning of Earth’s moisture recycling hubs

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Relevance of near-surface soil moisture vs. terrestrial water storage for global vegetation functioning

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Other Objects (12)

Relevance of near-surface soil moisture vs. terrestrial water storage for global vegetation functioning

Relevance of near-surface soil moisture vs. terrestrial water storage for global vegetation functioning

Relevance of near-surface soil moisture vs. terrestrial water storage for global vegetation functioning

Estimating Interception from Near-Surface Soil Moisture Response

Estimating root zone soil moisture using near-surface observations from SMOS

Global terrestrial moisture recycling in Shared Socioeconomic Pathways

Atmospheric moisture supersaturation in the near-surface atmosphere at Dome C, Antarctic Plateau

Changes in terrestrial near-surface wind speed and their possible causes: an overview

Large-scale vegetation responses to terrestrial moisture storage changes

Quantification of human contribution to soil moisture-based terrestrial aridity

The impact of near-surface soil moisture assimilation at subseasonal, seasonal, and inter-annual timescales

Network motifs shape distinct functioning of Earth’s moisture recycling hubs

Relevance of near-surface soil moisture vs. terrestrial water storage for global vegetation functioning

Relevance of near-surface soil moisture vs. terrestrial water storage for global vegetation functioning

Relevance of near-surface soil moisture vs. terrestrial water storage for global vegetation functioning

Estimating Interception from Near-Surface Soil Moisture Response

Estimating root zone soil moisture using near-surface observations from SMOS

Global terrestrial moisture recycling in Shared Socioeconomic Pathways

Atmospheric moisture supersaturation in the near-surface atmosphere at Dome C, Antarctic Plateau

Changes in terrestrial near-surface wind speed and their possible causes: an overview

Large-scale vegetation responses to terrestrial moisture storage changes

Quantification of human contribution to soil moisture-based terrestrial aridity

The impact of near-surface soil moisture assimilation at subseasonal, seasonal, and inter-annual timescales

Network motifs shape distinct functioning of Earth’s moisture recycling hubs

Relevance of near-surface soil moisture vs. terrestrial water storage for global vegetation functioning

Relevance of near-surface soil moisture vs. terrestrial water storage for global vegetation functioning

Relevance of near-surface soil moisture vs. terrestrial water storage for global vegetation functioning

Estimating Interception from Near-Surface Soil Moisture Response

Estimating root zone soil moisture using near-surface observations from SMOS

Global terrestrial moisture recycling in Shared Socioeconomic Pathways

Atmospheric moisture supersaturation in the near-surface atmosphere at Dome C, Antarctic Plateau

Changes in terrestrial near-surface wind speed and their possible causes: an overview

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Quantification of human contribution to soil moisture-based terrestrial aridity

The impact of near-surface soil moisture assimilation at subseasonal, seasonal, and inter-annual timescales

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