Articles | Volume 17, issue 10
https://doi.org/10.5194/hess-17-4269-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-17-4269-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
30 Oct 2013
Research article |
| 30 Oct 2013
Spatiotemporal characterization of dissolved carbon for inland waters in semi-humid/semi-arid region, China
K. S. Song
Department of Earth Sciences, Indiana University – Purdue University, Indianapolis, IN, USA
Northeast Institute of Geography and Agroecology, CAS, Changchun, China
S. Y. Zang
College of Geographical Science, Harbin Normal University, Harbin, China
Northeast Institute of Geography and Agroecology, CAS, Changchun, China
L. Li
Department of Earth Sciences, Indiana University – Purdue University, Indianapolis, IN, USA
J. Du
Northeast Institute of Geography and Agroecology, CAS, Changchun, China
N. N. Zhang
College of Geographical Science, Harbin Normal University, Harbin, China
X. D. Wang
College of Geographical Science, Harbin Normal University, Harbin, China
T. T. Shao
Northeast Institute of Geography and Agroecology, CAS, Changchun, China
Y. Guan
College of Geographical Science, Harbin Normal University, Harbin, China
L. Liu
College of Geographical Science, Harbin Normal University, Harbin, China
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Using daily ice records of 156 hydrological stations across Songhua River Basin, we examined the spatial variability in the river ice phenology and river ice thickness from 2010 to 2015 and explored the role of snow depth and air temperature on the ice thickness. Snow cover correlated with ice thickness significantly and positively when the freshwater was completely frozen. Cumulative air temperature of freezing provides a better predictor than the air temperature for ice thickness modeling.
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The study indicated that CDOM in rivers had higher aromaticity, molecular weight, and vascular plant contribution than in terminal lakes in the Hulun Buir plateau, Northeast China. The autochthonous sources of CDOM in plateau waters were higher than in other freshwater rivers reported in the literature. Study of the optical–physicochemical correlations is helpful in the evaluation of the potential influence of water quality factors on non-water light absorption in plateau water environments.
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During 1984–2018, lakes in the Tibetan-Qinghai Plateau had the clearest water (mean 3.32 ± 0.38 m), while those in the northeastern region had the lowest Secchi disk depth (SDD) (mean 0.60 ± 0.09 m). Among the 10 814 lakes with > 10 years of SDD results, 55.4 % and 3.5 % experienced significantly increasing and decreasing trends of SDD, respectively. With the exception of Inner Mongolia–Xinjiang, more than half of lakes in all the other regions exhibited a significant trend of increasing SDD.
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Using daily ice records of 156 hydrological stations across Songhua River Basin, we examined the spatial variability in the river ice phenology and river ice thickness from 2010 to 2015 and explored the role of snow depth and air temperature on the ice thickness. Snow cover correlated with ice thickness significantly and positively when the freshwater was completely frozen. Cumulative air temperature of freezing provides a better predictor than the air temperature for ice thickness modeling.
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Revised manuscript not accepted
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CDOM has strong link with DOC, which sets the basis for remote estimation of DOC in waters. However, the relationships between DOC and CDOM absorption for different types of inland waters may vary which worth further systematic investigations. Samples from fresh lakes, saline lakes, rivers, urban water bodies, ice-covered lakes were measured to examine the relationship between DOC and CDOM. The regression model slopes range from 1.03 for urban waters to 3.13 for river water.
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Our results of this study show that two humic-like C peaks and two protein-like B and T peaks were identified from CDOM using PARAFAC for investigated lakes. The average fluorescence intensity of the components differed seasonally. Components 1 and 2 exhibited strong linear correlation (R2 = 0.63). Significantly positive linear relationships, between aCDOM and Fmax, and between DOC and salinity (R2 = 0.93), were revealed.
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D. H. Mao, Z. M. Wang, L. Li, Z. H. Miao, W. H. Ma, C. C. Song, C. Y. Ren, and M. M. Jia
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The Sanjiang Plain of China, an important grain production base, is typical of ecosystems. In this study, 419 soil samples and a geostatistical method were used to estimate total SOC storage and to determine its pattern-controlling factors. The results from this study provide the most up-to-date knowledge on the storage and pattern of SOC in this plain, and the analysis conducted here could contribute to the determination of ecosystem carbon budgets and our understanding of ecosystem services.
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