Climate change, phenology, and phenological control of vegetation feedbacks to the climate system

被引:1630
作者
Richardson, Andrew D. [1 ]
Keenan, Trevor F. [1 ]
Migliavacca, Mirco [2 ]
Ryu, Youngryel [1 ,3 ]
Sonnentag, Oliver [1 ,4 ]
Toomey, Michael [1 ]
机构
[1] Harvard Univ, Dept Organism & Evolutionary Biol, HUH, Cambridge, MA 02138 USA
[2] Commiss European Communities, DG Joint Res Ctr, Inst Environm & Sustainabil, Climate Risk Management Unit TP290, I-21027 Ispra, VA, Italy
[3] Seoul Natl Univ, Dept Landscape Architecture & Rural Syst Engn, Seoul, South Korea
[4] Univ Montreal, Dept Geog, Montreal, PQ H2V 2B8, Canada
基金
美国国家科学基金会;
关键词
Autumn senescence; Biosphere-atmosphere interactions; Budburst; Carbon cycle; Climate change; Global warming; Models; Phenology; Seasonality; Spring onset; NET ECOSYSTEM PRODUCTIVITY; VOLATILE ORGANIC-COMPOUNDS; CARBON-DIOXIDE EXCHANGE; BOREAL ASPEN FOREST; LEAF BUD BURST; DECIDUOUS FOREST; INTERANNUAL VARIABILITY; PLANT PHENOLOGY; SEASONAL-VARIATION; SPRING PHENOLOGY;
D O I
10.1016/j.agrformet.2012.09.012
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Vegetation phenology is highly sensitive to climate change. Phenology also controls many feedbacks of vegetation to the climate system by influencing the seasonality of albedo, surface roughness length, canopy conductance, and fluxes of water, energy, CO2 and biogenic volatile organic compounds. In this review, we first discuss the environmental drivers of phenology, and the impacts of climate change on phenology, in different biomes. We then examine the vegetation-climate feedbacks that are mediated by phenology, and assess the potential impact on these feedbacks of shifts in phenology driven by climate change. We finish with an overview of phenological modeling and we suggest ways in which models might be improved using existing data sets. Several key weaknesses in our current understanding emerge from this analysis. First, we need a better understanding of the drivers of phenology, particularly in under-studied biomes (e.g. tropical forests). We do not have a mechanistic understanding of the role of photoperiod, even in well-studied biomes. In all biomes, the factors controlling senescence and dormancy are not well-documented. Second, for the most part (i.e. with the exception of phenology impacts on CO2 exchange) we have only a qualitative understanding of the feedbacks between vegetation and climate that are mediated by phenology. We need to quantify the magnitude of these feedbacks, and ensure that they are accurately reproduced by models. Third, we need to work towards a new understanding of phenological processes that enables progress beyond the modeling paradigms currently in use. Accurate representation of phenological processes in models that couple the land surface to the climate system is particularly important, especially when such models are being used to predict future climate. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:156 / 173
页数:18
相关论文
共 249 条
[1]   Drier summers cancel out the CO2 uptake enhancement induced by warmer springs [J].
Angert, A ;
Biraud, S ;
Bonfils, C ;
Henning, CC ;
Buermann, W ;
Pinzon, J ;
Tucker, CJ ;
Fung, I .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2005, 102 (31) :10823-10827
[2]  
[Anonymous], 1922, Q. J. R. Meteorolog. Soc.
[3]   Phenological data series of cherry tree flowering in Kyoto, Japan, and its application to reconstruction of springtime temperatures since the 9th century [J].
Aono, Yasuyuki ;
Kazui, Keiko .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2008, 28 (07) :905-914
[4]  
Archibald S, 2007, J VEG SCI, V18, P583, DOI 10.1658/1100-9233(2007)18[583:LGIASA]2.0.CO
[5]  
2
[6]  
Arft AM, 1999, ECOL MONOGR, V69, P491, DOI 10.1890/0012-9615(1999)069[0491:ROTPTE]2.0.CO
[7]  
2
[8]   Why are estimates of global terrestrial isoprene emissions so similar (and why is this not so for monoterpenes)? [J].
Arneth, A. ;
Monson, R. K. ;
Schurgers, G. ;
Niinemets, Ue. ;
Palmer, P. I. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2008, 8 (16) :4605-4620
[9]   Process-based estimates of terrestrial ecosystem isoprene emissions:: incorporating the effects of a direct CO2-isoprene interaction [J].
Arneth, A. ;
Niinemets, U. ;
Pressley, S. ;
Back, J. ;
Hari, P. ;
Karl, T. ;
Noe, S. ;
Prentice, I. C. ;
Serca, D. ;
Hickler, T. ;
Wolf, A. ;
Smith, B. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2007, 7 :31-53
[10]   A parameterization of leaf phenology for the terrestrial ecosystem component of climate models [J].
Arora, VK ;
Boer, GJ .
GLOBAL CHANGE BIOLOGY, 2005, 11 (01) :39-59