Abstract. Climate reconstructions provide important insight into
past climate variability and help us to understand the large-scale climate
drivers and impact of climate change. However, our knowledge about long-term
year-to-year climate variability is still limited due to the lack of
high-resolution reconstructions. Here, we present the first precipitation
reconstructions based on tree rings from Pinus koraiensis (Korean pine) from three sites
placed along a latitudinal (330 km) gradient in the Sikhote-Alin' mountains in the Russian Far East. The tree-ring width chronologies were built using standard
tree-ring procedures. We reconstructed the April–June precipitation for the
southern Sikhote-Alin' (SSA), March–June precipitation for the central
Sikhote-Alin' (CSA) and March–July precipitation for the northwestern
Sikhote-Alin' (NSA) over the years 1602 to 2013, 1804 to 2009 and 1858 to 2013, respectively. We found that an important limiting factor for Korean pine
growth was precipitation within the period when the air current coming from
the continent during the cold period is replaced with the impact of the wet
ocean air current. We identified that common wet years for SSA, CSA and NSA
occurred in 1805, 1853, 1877, 1903, 1906, 1927, 1983 and 2009 and common dry
years occurred in 1821, 1869, 1919, 1949 and 2003. Our reconstructions have
3-, 15- and 60-year periods, which suggests the influence of the El
Niño–Southern Oscillation and Pacific Decadal Oscillation on the
region's climate and relevant processes. Despite the impact of various
global processes, the main contribution to precipitation formation in the study
area is still made by the Pacific Ocean, which determines their amount and
periodicity.
Tree-ring-based spring precipitation reconstruction in the Sikhote-Alin' Mountain range
