I have excellent knowledge
of Hydrologic / Hydraulic s...
He is an expert in the application
of hydrologic and hydraulic numerical models to water resources infrastructure and regional watershed management.
Summary of Qualifications * Proven ability to provide sound and innovative engineering design services on schedule and at budget * Extensive experience in highway, municipal and land development design and permitting * Broad, in - depth knowledge
of hydrologic / hydraulic / stormwater modeling analysis and design * Strong motivational capacity, encouraging staff and satisfying clients» needs * Effectiveness in coordinating projec...
The approach is computationally efficient, allows for a greatly improved simulation
of the hydrologic cycle, and is easily coupled into the existing framework of the current generation of single column land - surface models.
Chapter 183 in: Encyclopedia
of the Hydrologic Sciences.
The early Eocene hyperthermals, a series of transient global warming events (2 to 5 °C, provide a unique opportunity to assess the sensitivity
of the hydrologic cycle to the scale of greenhouse forcing expected over the next several centuries.
For example, nearly all features
of the hydrologic system are now impacted by the Human System [60] with important feedbacks onto humans, e.g., snowpack decline due to climate change [53] reduces water availability; agricultural processes further affect water availability and water quality [54]; and land - use changes can reduce groundwater recharge [77].
J.
of Hydrologic Engineering, 1 - 14.
Here are examples of two papers that don't seem to have huge gaping flaws, and cover the data and the modeling
of hydrologic changes:
This report outlines the research activities
of the Hydrologic Impacts (HI) Theme for the period of 2015 - 2019.
Ablation measurements are repeated in late September at the designated conclusion
of the hydrologic year.
The only difference between the end result of the annual measurement programs is the difference in timing between the fixed date method and the end
of the hydrologic year method.
Journal
of Hydrologic Engineering 10.1 (2005): 8 - 15.
Together, the Colorado River flow, Southwest DAI, and southern Colorado Plateau temperature reconstructions allow an assessment of the covariation
of hydrologic drought with annual maximum temperatures, AD 762 — 1996.
Third, the special case
of a hydrologic watershed is particularly relevant to the water cycle and its availability for power and consumptive uses.
(Of course this is as simplistic as orange and blue balls — but it at least shows some understanding
of the hydrologic cycle and its effect on the energy flows rather than just looking at the overblown effects of CO2)
Abbott BW, Jones JB, Godsey SE, Larouche JR, Bowden WB (2015) Patterns and persistence
of hydrologic carbon and nutrient export from collapsing upland permafrost.
Now we are expanding our Data Portal again, with our new Gridded Hydrologic Model Output Page, which provides access to gridded, high - resolution projections
of hydrologic simulation data for four watersheds in British Columbia, generated at PCIC using the VIC hydrological model.
Important contribution to knowledge
of the hydrologic cycle, I think.
«Unlike common random series like those observed, for example, in games of chance, hydrologic (and other geophysical) time series have some structure, that is, consecutive values
of hydrologic time series depend on each other.
Every element
of the hydrologic cycle, to some degree, is temperature dependent: when it snows versus when it rains; when it melts, how much evaporates; how much water the plants use; the length of the growing seasons.
«In large part, the answer is that the basin has become hotter, which modifies several facets
of the hydrologic cycle that lie between precipitation and runoff, including evapotranspiration and sublimation rates, the timing of snowmelt and soil moisture characteristics,» according to the paper.
Markus leads the effort at PCIC to quantify the direct and indirect effects of climate change and variability upon the various components
of hydrologic cycle at the local and regional scale.
Evaluating the ability
of a hydrologic model to replicate hydro - ecologically relevant indicators.
During this time, Markus developed a clear and pragmatic appreciation
of the hydrologic effects of climate change and variability.
The aim
of the Hydrologic Impacts (HI) theme at PCIC is to quantify the effect of climate change and climate variability on regional hydrology in order to provide analysis and information relevant to water resources management.
Modelling spatial and temporal variability
of hydrologic impacts of climate change in the Fraser River basin, British Columbia, Canada.
The rainfall - evaporation interchange between the oceans and the atmosphere is by far the largest component
of the hydrologic cycle.
Extremes
of the hydrologic cycle are expected to intensify in a warmer world.
Hence, this study evaluates the ability of a standard hydrologic model set - up: Variable Infiltration Capacity (VIC) hydrologic model for two headwater sub-basins in the Fraser River (Salmon and Willow), British Columbia, Canada, with climate inputs derived from observations and statistically downscaled global climate models (GCMs); to simulate six general water resource indicators (WRIs) and 32 ecologically relevant indicators
of hydrologic alterations (IHA).
The result of putting more carbon into the atmosphere than can be taken out of it is a warmer climate, a melting Arctic, higher sea levels, improvements in the photosynthetic efficiency of many plants, an intensification
of the hydrologic cycle of evaporation and precipitation, and new ocean chemistry.
Many impacts settings are somewhat tuned to a certain resolution, such as the nested size categorizations
of hydrologic basins down to watershed size, commonly used in hydrologic modeling.
Application of the VIC model and the generation
of hydrologic projections for the Peace, Fraser, upper Columbia and Campbell River watersheds are described in Shrestha et al. (2012) and Schnorbus et al. (2011, 2014).
Shrestha, R. R., M. A. Schnorbus, A. T. Werner, and A. J. Berland, 2012: Modelling spatial and temporal variability
of hydrologic impacts of climate change in the Fraser River basin, British Columbia, Canada.
The principal scientific objective is to make global SSS measurements over the ice - free oceans with 150 - km spatial resolution, and to achieve a measurement error less than 0.2 (PSS - 78 [practical salinity scale of 1978]-RRB- on a 30 - day time scale, taking into account all sensors and geophysical random errors and biases.Salinity is indeed a key indicator of the strength
of the hydrologic cycle because it tracks the differences created by varying evaporation and precipitation, runoff, and ice processes.
A realistic treatment
of the hydrologic cycle would show that the influence of a doubling of CO2 should lead to a global surface warming of only about 0.3 °C — not the 3 °C warming as indicated by the climate simulations....
Energetic constraints and response
of hydrologic cycle to climate change.
Also, just because the average pole - to - equator temperature gradient is decreasing doesn't mean that the seasonal variation won't still be in place, and then there's the whole issue
of the hydrologic cycle intensification — a moister atmosphere carries more latent heat and thus may generate more intense mid-latitude storms as well.
Note also that there appears — already started — to be a likely increase in drought frequency with atmospheric warming and associated acceleration
of the hydrologic cycle, assuming continued greenhouse gas emissions.
This aspect
of the hydrologic cycle was recognized by the 2005 National Research Council report (see pages 93 - 98 in http://www.nap.edu/openbook/0309095069/html/) as a non-radiative climate forcing.
To my mind the more important result of this review paper was in the synthesis of information from many discipines that point towards an ongoing intensification
of the hydrologic cycle — not that I did not find evidence for more frequent or intense storms.
It made me curious if there might not have been a relationship to the volcanic activity in the Caribbean in the late 90's and the possible character
of the hydrologic cycle in the early 90's.
Calibration
of hydrologic models is limited by the length of the historical river data.
While most literature emphasises that the increasing magnitude of storm rainfall extends beyond the original protection standards
of hydrologic facilities in highly populated delta cities.
What is Irrigation, Necessity of Irrigation, Advantages and disadvantages of Irrigation - Irrigation can be defined as human manipulation
of the hydrologic While nanotechnology is seen as the way of the future and is a technology that a lot of people think will bring a lot of benefit for all who will be using it,
They have provided a much better understanding
of hydrologic responses to climate change, which in turn will provide tremendous guidance for future planning.»
Extremes
of the hydrologic cycle are expected to intensify in a warmer world.
10:30 - 10:45 Reconstructing the past millennium
of hydrologic variability in the Western Tropical Pacific using the hydrogen isotopes of lipid biomarkers Julie Richey, Julian Sachs
Chapter C: Numerical Model
of the Hydrologic Landscape and Groundwater Flow in California's Central Valley.
The Consortium of Universities for the Advancement
of Hydrologic Science (CUAHSI) hosts the public database with funding from the National Science Foundation (NSF).