Lecture 04 Water-rock interaction will come later

Slides:

Advertisements

Similar presentations

Spruce W. Schoenemann UWHS Atmospheric Sciences 211 May 2013 Dept. of Earth and Space Sciences University of Washington Seattle From Isotopes.

Advertisements

Paleoceanography Antarctica Circumpolar Current:.

Mark Williams, CU-Boulder What causes different isotopic values in source waters and flowpaths?

Water Isotopes in the Hydrosphere I10/10/05 Lecture outline: 1)the hydrological cycle  D and  18 O variability 3)fractionation processes  18 O,

Isotope mass balance – Mica Creek Paul Koeniger, Tim Link, John Marshall 03/28/2006 – Mica Creek Group Meeting Department of Forest Resources – University.

Co 2 sequestration and AJAX. atmospheric CO 2 - increase roughly matches amount, rate and isotopic ratio ( 13 C, 12 C) expected from burning “fossil”

Engineering Hydrology (ECIV 4323)

Lecture 04 Water-rock interaction will come later

Water in the Air When water drops form on a cold glass, the water comes from the air around the glass. Water vapor is water in the form of a gas. The amount.

Integrated Approach for Assessing the Characteristic of Groundwater Recharge in Basin Scale Hsin-Fu Yeh*, Cheng-Haw Lee, Kuo-Chin Hsu Department of Resources.

8.1/8.2 Climate Change Weather and Climate. Weather Atmospheric conditions in a particular location over a short period of time Includes: temperature,

The Water cycle By Amy Connie Gardner Capstone 2 Performance Indicator 1C Evidence-student sample.

David Schneider and Eric Steig Isotopic Records in US-ITASE Cores: A preliminary report WAIS Workshop September, 2003 University of Washington.

4 th Grade Weather and Water Cycle Vocabulary Mrs. Thornburg’s version.

Paleoclimatology Why is it important? Angela Colbert Climate Modeling Group October 24, 2011.

Ice Cores Very important paleoclimatic archives. Records of past atmospheric conditions. –Temperature –Humidity –Snow accumulation –Atmospheric composition.

Run-Off Characteristics of Streams

Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1.

Advancements in Simulating Land Hydrologic Processes for Land Surface Modeling (LSM) Hua Su Presentation for Physical Climatology.

Signals of climate change and the Southern Annular Mode in Antarctic stable isotope records David P. Schneider and Eric J. Steig Department of Earth and.

Effects of different surface types and human activities.

Sea Level Change Concept Maps. Overview Overarching Concept: Changes in sea level have occurred in the past, are occurring now, and will continue to occur.

Figure 6-1. Graphical representation of decay of radioactive parent (N) and growth of radiogenic progeny (P).

Atmosphere and Weather Patterns Taylor Science

Chemistry Unit. Properties of Water and their Relationship to Weather and Climate.

Table of Contents  The Water Cycle The Water Cycle The Water Cycle  June 2005 Rainfall June 2005 Rainfall June 2005 Rainfall  June 2005 Weather June.

CE 424 HYDROLOGY 1 Instructor: Dr. Saleh A. AlHassoun.

Quality control of daily data on example of Central European series of air temperature, relative humidity and precipitation P. Štěpánek (1), P. Zahradníček.

Engineering Hydrology (ECIV 4323)

Lecture 8 Evapotranspiration (1) Evaporation Processes General Comments Physical Characteristics Free Water Surface (the simplest case) Approaches to Evaporation.

Ch.3. Precipitation  The significance of precipitation data? Basis for all the hydrological evaluation  The T-  18 O Correlation in Precipitation For.

Spatial Interpolation Chapter 13. Introduction Land surface in Chapter 13 Land surface in Chapter 13 Also a non-existing surface, but visualized as a.

ORCHIDEE-Dev : January 8th, 2013 Theme #1 Water cycle, river flows, water quality and interactions with biosphere under future climate Réservoir souterrain.

Incorporation of Stable Water Isotopes in GSM and Spectrum-Nudged 28-year Simulation Kei YOSHIMURA 1,2 1: Scripps Institution of Oceanography, University.

Program Outline LECTURE 1 – Introduction to Isotopes LECTURE 2 – Characteristics of different isotope systems – Mostly home study LECTURE 3 – Meteoric.

Concept of Humidity What is the relationship between water vapor holding and temperature? Air hold more water vapour at higher temperature.

Seasonal and elevational variation of surface water  18 O and  2 H in the Willamette River basin J. Renée Brooks 1, Parker J. Wigington 1, Jr., Carol.

Unit 11 Lesson 2 Elements of Weather

1. The atmosphere 2 © Zanichelli editore 2015 Characteristics of the atmosphere 3 © Zanichelli editore 2015.

Incorporating Stable Water Isotopes in the Community Land Model Xinping Zhang 1 Guoyue Niu 2 Zongliang Yang 2 1 College of Resources and Environmental.

The Earth is surrounded by a thin blanket of air called the atmosphere.

Teaching Point: “To analyze the moisture in the atmosphere” Do Now Discussion: Turn to page 14 of your ESRT. How does water vapor and altitude in the atmosphere.

Topic: Water in the Atmosphere PSSA: C / S8.D.2.1.

Water Cycle, Cloud Formation, and Severe Weather.

Weather & Climate air pressure the weight of air.

Ch.2. Tracing the Hydrological Cycle  Craig’s meteroic relationship in global fresh water  D = 8  18 O + 10 ‰ SMOW (Craig, 1961)  From IAEA-GNIP 

What are the three main cloud types?

ELEC-E3151 Mathematical Computing

第四節氢穩定同位素氢同位素的基本特征测量方法国际标准分馏系数常见应用.

Lecture 8 Evapotranspiration (1)

Let’s Get Ready to Play!!.

Engineering Hydrology (ECIV 4323)

Earth Science SAGE Workbook SAGE Review

Equilibrium fractionation

The Hydrosphere Lecture 04 Chapter 4.

SCIENCE GRADE FOUR – WEATHER

Multiple Regression A curvilinear relationship between one variable and the values of two or more other independent variables. Y = intercept + (slope1.

Introduction to Meteorology

Chapter 9 Meteorology.

Engineering Hydrology (ECIV 4323)

Engineering Hydrology (ECIV 4323)

Review for Chapter 5 Test

Cases. Simple Regression Linear Multiple Regression.

Humidity and Water Vapor

Weather Vocabulary.

The Importance of Water

Presentation transcript:

Lecture 04 Water-rock interaction will come later The Hydrosphere Lecture 04 Water-rock interaction will come later

The isotope water cycle

Global Meteoric Water Line

Evaporation

Evaporation of small reservoir

Evaporation of finite reservoir

Evaporation of infinite reservoir

Evaporation slopes

Deuterium excess and relative humidity

Local Meteoric Water Lines

Rayleigh Distillation

IAEA GNIP Stations

Global Distribution From Bowen, Geology. Bowen, G.J. and Wilkinson, B., 2002. Spatial distribution of delta O-18 in meteoric precipitation. Geology, 30(4): 315-318.

Temperature Effect Clark and Fritz, p. 65

Continental effect

Continental effect

A real example

Altitude effect

Altitude effect

Altitude gradients

Amount effect

Source effect

Seasonal effect

Seasonal/Source effect at LAS

Isoscapes Based on Multiple regression analysis of linear correlations to climate/physiographic parameters Or… Contouring/kriging (spatial interpolation).