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Elevation-dependent sensitivity of spectral greening to temperature and precipitation in the Western Himalayas

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985939%3A_____%2F25%3A00619836" target="_blank" >RIV/67985939:_____/25:00619836 - isvavai.cz</a>

  • Nalezeny alternativní kódy

    RIV/60076658:12310/25:43911221

  • Výsledek na webu

    <a href="https://iopscience.iop.org/article/10.1088/1748-9326/adc9c7" target="_blank" >https://iopscience.iop.org/article/10.1088/1748-9326/adc9c7</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1088/1748-9326/adc9c7" target="_blank" >10.1088/1748-9326/adc9c7</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Elevation-dependent sensitivity of spectral greening to temperature and precipitation in the Western Himalayas

  • Popis výsledku v původním jazyce

    Mountain ecosystems are experiencing significant changes due to climate change. Globally, a prevailing greening trend has been observed over the past decades using remote-sensing normalized difference vegetation index (NDVI), suggesting increasing vegetation cover and primary productivity. However, NDVI responses to warming differ across regions. Cold, energy-limited alpine and tundra ecosystems tend to respond positively to warming, while arid, water-limited ecosystems may experience reduced NDVI due to higher transpiration rates limiting plant growth. Additionally, CO2 fertilization effect enhances vegetation productivity by improving plant water use efficiency. This study investigates the drivers of temporal trends in annual maximum NDVI (NDVImax) along an elevational gradient in the arid Western Himalaya (Ladakh, India). We hypothesize that NDVImax will be more sensitive to precipitation anomalies at lower elevations, whereas at higher elevations it will be more sensitive to temperature anomalies. Using Landsat satellite data from 2001 to 2022, we related NDVImax temporal anomalies to temperature and precipitation obtained from the ERA5-Land reanalysis dataset, and local snow cover from MODIS. Our results show complex interactions between climate and elevation that influence NDVImax. Contrary to our expectations, precipitation exhibited a strong positive effect on NDVImax across all elevations and seasons, except for autumn at higher elevations. Temperature effects were weaker and varied across seasons and elevations. Higher summer temperatures increased NDVImax at higher elevations but decreased it at lower elevations. We observed a multidecadal greening trend independent of temperature and precipitation, with this greening being more pronounced at lower elevations. This study highlights the importance of context dependency in understanding vegetation dynamics in fragile, low-productivity mountain ecosystems.

  • Název v anglickém jazyce

    Elevation-dependent sensitivity of spectral greening to temperature and precipitation in the Western Himalayas

  • Popis výsledku anglicky

    Mountain ecosystems are experiencing significant changes due to climate change. Globally, a prevailing greening trend has been observed over the past decades using remote-sensing normalized difference vegetation index (NDVI), suggesting increasing vegetation cover and primary productivity. However, NDVI responses to warming differ across regions. Cold, energy-limited alpine and tundra ecosystems tend to respond positively to warming, while arid, water-limited ecosystems may experience reduced NDVI due to higher transpiration rates limiting plant growth. Additionally, CO2 fertilization effect enhances vegetation productivity by improving plant water use efficiency. This study investigates the drivers of temporal trends in annual maximum NDVI (NDVImax) along an elevational gradient in the arid Western Himalaya (Ladakh, India). We hypothesize that NDVImax will be more sensitive to precipitation anomalies at lower elevations, whereas at higher elevations it will be more sensitive to temperature anomalies. Using Landsat satellite data from 2001 to 2022, we related NDVImax temporal anomalies to temperature and precipitation obtained from the ERA5-Land reanalysis dataset, and local snow cover from MODIS. Our results show complex interactions between climate and elevation that influence NDVImax. Contrary to our expectations, precipitation exhibited a strong positive effect on NDVImax across all elevations and seasons, except for autumn at higher elevations. Temperature effects were weaker and varied across seasons and elevations. Higher summer temperatures increased NDVImax at higher elevations but decreased it at lower elevations. We observed a multidecadal greening trend independent of temperature and precipitation, with this greening being more pronounced at lower elevations. This study highlights the importance of context dependency in understanding vegetation dynamics in fragile, low-productivity mountain ecosystems.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10511 - Environmental sciences (social aspects to be 5.7)

Návaznosti výsledku

  • Projekt

    <a href="/cs/project/GA24-11954S" target="_blank" >GA24-11954S: Alpinské rostliny a změna klimatu: od adaptačních strategií k fungování ekosystémů</a><br>

  • Návaznosti

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Ostatní

  • Rok uplatnění

    2025

  • Kód důvěrnosti údajů

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Údaje specifické pro druh výsledku

  • Název periodika

    Environmental Research Letters

  • ISSN

    1748-9326

  • e-ISSN

    1748-9326

  • Svazek periodika

    20

  • Číslo periodika v rámci svazku

    5

  • Stát vydavatele periodika

    GB - Spojené království Velké Británie a Severního Irska

  • Počet stran výsledku

    11

  • Strana od-do

    054078

  • Kód UT WoS článku

    001487310900001

  • EID výsledku v databázi Scopus

    2-s2.0-105005144307