BEGIN:VCALENDAR
VERSION:2.0
PRODID:-//www.bayceer.uni-bayreuth.de//NONSGML kigkonsult.se iCalcreator 2.41.92//
CALSCALE:GREGORIAN
METHOD:PUBLISH
UID:62636161-3532-4361-a533-333930613038
X-WR-CALNAME:BayCMS-Export
X-WR-CALDESC:This is a calendar exported from BayCMS
X-WR-TIMEZONE:Europe/Berlin
BEGIN:VTIMEZONE
TZID:Europe/Berlin
TZUNTIL:20100328T010000Z
BEGIN:STANDARD
TZNAME:CET
DTSTART:20071028T030000
TZOFFSETFROM:+0200
TZOFFSETTO:+0100
RDATE:20081026T030000
RDATE:20091025T030000
END:STANDARD
BEGIN:DAYLIGHT
TZNAME:CEST
DTSTART:20080330T020000
TZOFFSETFROM:+0100
TZOFFSETTO:+0200
RDATE:20090329T020000
END:DAYLIGHT
END:VTIMEZONE
BEGIN:VEVENT
UID:www.bayceer.uni-bayreuth.de-bayceer-t60368id
DTSTAMP:20260817T100931Z
DESCRIPTION:Recent improvements in both automated temperature-data acquisit
 ion and simulation modeling of heat and ground-water transport\, are leadi
 ng to widespread implementation of heat as a tracer of ground-water fluxes
  near streams. The presentation provides a brief historical review of the 
 use of heat as a tracer of shallow ground-water movement\, and details cur
 rent theory used to estimate stream exchanges with ground water. The gover
 ning equations for heat and ground-water transport in the near-stream envi
 ronment are presented. The various relations between the hydrologic state 
 of a stream channel and the expected thermal response is graphical depicte
 d. Techniques for installation and monitoring of temperature and stage equ
 ipment are discussed for a range of hydrological environments. These techn
 iques are divided into direct measurement techniques in streams and sedime
 nts\, indirect techniques relying on near-stream observation wells\, and r
 emote sensing and other technically advanced temperature acquisition techn
 iques. As a result presumably of a natural sense of heat\, temperature is 
 graphical visualized more often and diversely than other environmental par
 ameters. Visualizations of stream and streambed temperature patterns are d
 iscussed using thermographs\, temperature envelopes\, and 1-\, 2-\, and 3-
 dimensional temperature contour plots. Methods of analysis of observed tem
 peratures include simple heat-pulse arrival-time and heat-loss procedures\
 , analytical and time-series solutions\, and heat and water transport simu
 lation models. Applications of heat as tracer are presented for a variety 
 of stream sites\, ranging from a large bank filtration facility on the Rus
 sian River in northern California to ephemeral arroyos (wadis) in the dese
 rt Southwest bordering Mexico.
DTSTART;TZID=Europe/Berlin:20080519T141500
DTEND;TZID=Europe/Berlin:20080519T235959
LOCATION:H 6
SUMMARY:Dr. Jim Constantz\, U.S. Geological Survey\, Menlo Park\, Californi
 a: Heat as a Tracer of Stream Exchanges with Ground Water
TRANSP:TRANSPARENT
END:VEVENT
END:VCALENDAR