Intraseasonal Interactions between Temperature and Vegetation over the Boreal Forests

نویسندگان

  • Weile Wang
  • Bruce T. Anderson
  • Dara Entekhabi
  • Dong Huang
  • Yin Su
  • Robert K. Kaufmann
  • Ranga B. Myneni
  • Ralph M. Parsons
چکیده

This paper uses statistical and analytical techniques to investigate intraseasonal interactions between temperature and vegetation [surrogated by the normalized difference vegetation index (NDVI)] over the boreal forests. Results indicate that interactions between the two fields may be approximated as a coupled second-order system, in which the variability of NDVI and temperature of the current month is significantly regulated by lagged NDVI anomalies from the preceding two months. In particular, the influence from the one-month lagged NDVI anomalies upon both temperature and vegetation variability is generally positive, but the influence from the second-month lagged NDVI anomalies is often negative. Such regulations lead to an intrinsic oscillatory variability of vegetation at growing-season time scales across the study domain. The regulation of temperature variability by NDVI anomalies is most significant over interior Asia (Siberia), suggesting strong vegetation–atmosphere couplings over these regions. Physical mechanisms for these statistical results are investigated further with a stochastic model. The model suggests that the oscillatory variability of the temperature–NDVI system may reflect the dynamic adjustments between the two fields as they maintain a thermal balance within the soil and lower boundary layer of the atmosphere; the particular role vegetation plays in this scenario is mainly to dissipate heat and therefore reduce surface temperatures.

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Linking sediment-charcoal records and ecological modeling to understand causes of fire-regime change in boreal forests.

Interactions between vegetation and fire have the potential to overshadow direct effects of climate change on fire regimes in boreal forests of North America. We develop methods to compare sediment-charcoal records with fire regimes simulated by an ecologica model, ALFRESCO (Alaskan Frame-based Ecosystem Code) and apply these methods to evaluate potential causes of a mid-Holocene fire-regime sh...

متن کامل

Divergent Arctic-Boreal Vegetation Changes between North America and Eurasia over the Past 30 Years

Arctic-Boreal region—mainly consisting of tundra, shrub lands, and boreal forests—has been experiencing an amplified warming over the past 30 years. As the main driving force of vegetation growth in the north, temperature exhibits tight coupling with the Normalized Difference Vegetation Index (NDVI)—a proxy to photosynthetic activity. However, the comparison between North America (NA) and north...

متن کامل

Biomass Estimation for Boreal Forests Using Field, Lidar and L-band Sar Data

The coupling of LIDAR and SAR for vegetation structure has been investigated in several terrestrial biomes [7, 4, 6]. In this paper, we explore the measurement of biomass in boreal forests. This ecosystem was selected since the boreal biome is environmentally important, yet significantly under-sampled. The boreal forest biome consists of a circumpolar region lying above 50o–60o latitude and ext...

متن کامل

Temperature and vegetation seasonality diminishment over northern lands - xu-myneni-msp

Global temperature is increasing, especially over northern lands (> 50 ◦ N), owing to positive feedbacks1. As this in-­‐ crease is most pronounced in winter, temperature seasonality (ST)—conventionally defined as the difference between sum-­‐ mer and winter temperatures—is diminishing over time2, a phenomenon that is analogous to its equatorward decline at an annual scale. The initiation, termi...

متن کامل

Interactions with successional stage and nutrient status determines the life-form-specific effects of increased soil temperature on boreal forest floor vegetation

The boreal forest is one of the largest terrestrial biomes and plays a key role for the global carbon balance and climate. The forest floor vegetation has a strong influence on the carbon and nitrogen cycles of the forests and is sensitive to changes in temperature conditions and nutrient availability. Additionally, the effects of climate warming on forest floor vegetation have been suggested t...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

عنوان ژورنال:

دوره   شماره 

صفحات  -

تاریخ انتشار 2007