More Like this

1. Long‐term hydrology and aquatic biogeochemistry data from H. J. Andrews Experimental Forest, Cascade Mountains, Oregon

   https://doi.org/10.1002/hyp.14187  

   Johnson, Sherri L. ; Henshaw, Don ; Downing, Greg ; Wondzell, Steve ; Schulze, Mark ; Kennedy, Adam ; Cohn, Greg ; Schmidt, Stephanie A. ; Jones, Julia A. ( May 2021 , Hydrological Processes)
2. The large-scale, long-term coupling of temperature, hydrology, and water isotopes

   https://doi.org/10.1175/JCLI-D-20-0563.1  

   Siler, Nicholas ; Bailey, Adriana ; Roe, Gerard H. ; Buizert, Christo ; Markle, Bradley ; Noone, David ( May 2021 , Journal of Climate)

   null (Ed.)

   Abstract The stable isotope ratios of oxygen and hydrogen in polar ice cores are known to record environmental change, and they have been widely used as a paleothermometer. Although it is known to be a simplification, the relationship is often explained by invoking a single condensation pathway with progressive distillation to the temperature at the location of the ice core. In reality, the physical factors are complicated, and recent studies have identified robust aspects of the hydrologic cycle’s response to climate change that could influence the isotope-temperature relationship. In this study, we introduce a new zonal-mean isotope model derived from radiative transfer theory, and incorporate it into a recently developed moist energy balance climate model (MEBM), thus providing an internally consistent representation of the tight physical coupling between temperature, hydrology, and isotope ratios in the zonal-mean climate. The isotope model reproduces the observed pattern of meteoric δ 18 O in the modern climate, and allows us to evaluate the relative importance of different processes for the temporal correlation between δ 18 O and temperature at high latitudes. We find that the positive temporal correlation in polar ice cores is predominantly a result of suppressed high-latitude evaporation with cooling, rather thanmore »local temperature changes. The same mechanism also explains the difference in the strength of the isotope-temperature relationship between Greenland and Antarctica.« less
3. Linking Hydrology and Dissolved Organic Matter Characteristics in a Subtropical Wetland: A Long‐Term Study of the Florida Everglades

   https://doi.org/10.1029/2020GB006648  

   Regier, Peter ; Larsen, Laurel ; Cawley, Kaelin ; Jaffé, Rudolf ( December 2020 , Global Biogeochemical Cycles)
4. Constructing a long-term monthly climate data set in central Asia: CONSTRUCTING A LONG-TERM MONTHLY CLIMATE DATA SET IN CENTRAL ASIA

   https://doi.org/10.1002/joc.5259  

   Zhou, Hang ; Aizen, Elena ; Aizen, Vladimir ( March 2018 , International Journal of Climatology)
5. How do data collection and processing methods impact the accuracy of long-term trend estimation in lake surface-water temperatures?: Estimating long-term lake temperature trends

   https://doi.org/10.1002/lom3.10262  

   Gray, Derek K. ; Hampton, Stephanie E. ; O'Reilly, Catherine M. ; Sharma, Sapna ; Cohen, Rachel S. ( August 2018 , Limnology and Oceanography: Methods)