| Live Updates Below and see new post | Richard Muller, a cantankerous but creative physicist at the University of California, Berkeley, who once derided climate change research, then dove in with his own reconstruction of terrestrial temperature changes and confirmed substantial warming, has now concluded that recent warming is "almost entirely" human caused.
We used the annual growth rate of a stalagmite (XL21) collected from Xianglong Cave, central China, to quantitatively reconstruct regional terrestrial temperature changes over the last 95 years (1912 2006 AD).
Land surface temperature (LST), a key parameter in understanding thermal behavior of various terrestrial processes, changes rapidly and hence mapping and modeling its spatio-temporal evolution requires measurements at frequent intervals and finer resolutions.
Here we discuss paleoenvironmental evolution in the Baikal region during the Holocene using new records of aquatic (diatom) and terrestrial vegetation changes from Hovsgol, Mongolia's largest and deepest lake.
This may arise because mysids are exposed to greater marine-derived carbon sources later in the summer, a decrease in freshwater input (and hence terrestrial carbon), changes in phytoplankton or macrophyte community structure, or that mysids preferentially feed on marine food sources.
2012), while in terrestrial species changes in gait posture that redistribute weight across the limbs can explain such reduced manoeuvrability with body mass (Heglund & Taylor 1988; Biewener 2003).
Large areas of natural and anthropogenic land cover change are closely related to the interaction of the cryosphere and terrestrial hydrology change (Tchebakova et al. 2009; Zhang et al. 2011, Mátyás and Sun 2014; Fig. 4) with human activities (Qi et al. 2012, 2012; Chen et al. 2013, 2015; Horion et al. 2016, Figs. 12 and 15).
The complexities of terrestrial surface change demand a theoretical overview that is both flexible and multifaceted.
Scientists can show how the areas of oceans, marginal seas, and terrestrial basins change with elevation and depth using a special curve known as a hypsometric, or hypsographic, curve.
Terrestrial storage change is more capable of accommodating climatic fluctuations at the intra-annual scale than at the interannual scale, and for some arid regions it is the dominant factor influencing the E variance.
The motivations for this work is to understand the relationship between Gravity Recovery and Climate Experiment (GRACE) derived terrestrial water change (ΔTWS) data and GWL, so that ΔTWS could be used as a proxy measurement for GWL.
