Heavy Precipitation and High Streamflow in the Contiguous United States: Trends in the Twentieth Century.
By P. Groisman, R. Knight, Thomas Karl. 2001
494 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Water Science and Technology
View Paper: https://www.semanticscholar.org/paper/881c0de6089e788f274862b882a6f0d379cf7df0
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- Marc B. Parlange
- Philippe Naveau
- Ajay Kalra
- F. Zwiers
- Shandar Ahmad
- R. Katz
- Xuebin Zhang
- Fernando Port'e-Agel
In Global and Planetary Change
In Water Science and Technology
Citations in the corpus
- Climate change and changes in global precipitation patterns: what do we know? (2005, background): “This has been further evaluated by Groisman et al. (2001), who show that changes in snowcover extent also influence the timing and volume of streamflow.”
- Statistics of extremes in hydrology (2002, background): “As part of global climate change, an accelerated hydrologic cycle (including an increase in heavy precipitation) is anticipated on a theoretical basis [95,96], is predicted by numerical models of the climate system [21], and has been detected in observed precipitation [32,48] and, possibly, streamfl”
- Using oceanic‐atmospheric oscillations for long lead time streamflow forecasting (2007, background): “Trends in streamflow [Groisman et al., 2001; Kalra et al., 2008] are important as they help the water managers in responding to changes in water supply.”
- Use of a nonstationary copula to predict future bivariate low flow frequency in the Connecticut river basin (2016, background): “Groisman et al. (2001) concluded that high flows in the eastern U.S. increased as a result of increasing precipitation.”
- Monte Carlo experiments on the detection of trends in extreme values (2004, background): “This observation has motivated many studies of extremes in the climate of the twentieth century (e.g., Groisman et al. 2001; Iwashima and Yamamoto 1993; Kunkel et al. 1999; Zhang et al. 2001a,b) and in the climate projected for the twenty-first century (e.g., Zwiers and Kharin 1998; Kharin and…”