Moreover, field studies have rarely reported the pH and
temperature of water samples, which could have a big effect on true concentrations of contaminants.
Not exact matches
Kaustubh Thirumalai (Brown University) helping retrieve a CTD instrument, which collects
water samples and measures physical parameters
of oceanic
waters such as
temperature, aboard the R / V Point Sur in the northern Gulf
of Mexico.
MELISA consists
of a
water bath heater that incubates
samples at a target
temperature and analyzes them via images taken by mobile phone.
Measuring -
Temperature and Thermometers Classifying Components
of Mixtures Predicting - Surveying Opinion SAPA Part C, Directions for the Multiplication Game SAPA Part C and E, Multiplication Game SAPA Part D 1st Draft, c. 1972 The Whirling Dervish The Bouncing Ball The Effect
of Liquid on Living Tissue Rate
of Change Observing Growth from Seeds An Intro to Scales Forces on Static and Moving Objects Observations and Inferences Using Punch Cards to Record a Classification Using Maps to Describe Location A Tree Diary SAPA Part D 2nd Draft Observations and Inferences The Bouncing Ball Rate
of Change A Tree Diary An Intro to Scales and Scaling Observing Growth from Seeds (The Bean - It Came Up) Forces on Static and Moving Objects Using Punch Cards to Record a Classification Relative Position and Motion Inferring - The
Water Cycle Predicting 4 - The Suffocating Candle The Big Cleanup Campaign 2 - D Representation
of Spatial Figures Using Maps to Describe Location SAPA Part D Tryout Draft, 1972 Observations and Inferences The Bouncing Ball Measuring Drop by Drop Rate
of Change Predicting 4 - The Suffocating Candle Forces on Static and Movign Objects Observing Growth from Seeds Using Space / Time Relationships -2-D Representation
of Spatial Figures Using Punch Cards to Record a Classification An Introduction to Scales and Scaling The Effect
of Liquid on Living Tissue Inferring - The
Water Cycle Relative Position and Motion Using Maps to Describe Location The Big Cleanup Campaign A Tree Diary SAPA II Module (s), c. 1973 1, Tentative Format
Sample, Perception
of Color 9, Sets and Their Members 6, Direction and Movement, Draft 34, About How Far?
Some
of the
samples sat in freezers, others under the sink, and still others in
water baths maintained at various
temperatures.
For this particular research, the scientists tested
samples of common salt — sodium chloride — along with mixtures
of salt and
water, in their vacuum chamber at Europa's chilly surface
temperature of minus 280 degrees Fahrenheit (minus 173 Celsius).
«As the observed NMR signal is proportional to the amount
of ortho -
water in the
sample (para-
water «NMR silent»), we can track the percentages
of ortho and para isomers at any time and any
temperature,» Mamone explained.
Kelsey Poulson - Ellestad, a former graduate student at the Georgia Institute
of Technology, now at Woods Hole Oceanographic Institution, works with a Conductivity,
temperature and depth (CTD)
sampling rosette, which is lowered over the side
of a vessel and is used to collect
water samples from various depths.
The ability to peek into the process
of splitting
water at room
temperature has been hindered by the fact that most imaging or crystallography technology using X-ray lasers blasts the
samples to bits before meaningful data can be collected.
We present such a relationship for aragonite saturation state for
waters off Northern California based on in situ bottle
sampling and instrumental measurements
of temperature, salinity, and dissolved oxygen.
As the space filled to capacity and the
temperature began to rise — with nary a beer, wine, or
water in the offing — I roped artist Emily Harris into the compare - and - contrast exercise
of sampling a couple
of other local openings.
News that SST
temperature readings are kaput because
of differences in methods
of drawing sea
water samples are highly exaggerated, to paraphrase Mark Twain.
It is widely realized that WWii saw changes in the construction
of sampling buckets for sea surface
temperature measurement, and many navies switching to
water intake
temperatures in compiling data from ships at sea.
Clearly a lot
of sampling skill is needed to discount trees that have taken root where subsoil variability comes into play, lest that inhomogeneity
of nutrient and
water availability blur or wash out the
temperature component.
A couple
of years ago I went out with my rowing boat (I live 100 yards from the sea) and took
water samples in a container from various depths and measured the
temperature after leaving the
water in the bucket for various timings.
If scientists need to rely on bucket
samples of water to prove the historic global
temperature of our oceans, perhaps it is time to recognise that there are some aspects
of our climate data that are not worth relying on.
One
of my introductions to the strange world
of climatism was a discussion at Climate Audit, where Steve McIntyre and his colleagues were trying to puzzle out the effect
of a changeover in the early 20th century from leather to oaken buckets for gathering
water samples for measuring ocean
temperature.
The new ERSST4
temperature series includes an» (i) an increasing amount
of ocean data from buoys, which are slightly different than data from ships; (ii) an increasing amount
of ship data from engine intake thermometers, which are slightly different than data from bucket sea -
water temperatures; and (iii) a large increase in land - station data...» and «More generally, buoy data have been proven to be more accurate and reliable than ship data, with better known instrument characteristics and automated
sampling.»
If the bucket were dragged at
sampling depth for a few minutes before extraction, the walls
of the bucket would have come near the ambient
water temperature, slowing heat loss from the captured
water.
There is contamination
of the air in the bubble by
water; different results are obtained if the ice is crushed or melted to obtain the air
sample; it takes decades for the air bubble to form; the raw data was smoothed out by a 70 year moving average that removed the great annual variability found in the 19th century and Stomata Index (SI) records; closer examination revealed a major flaw in the hypothesis because
temperature rises before CO2.
Some billions
of dollars later, your lab assistant tells you that the
water sample you used was actually 33 K before you applied the energy that resulted in a final
temperature of 288 K.
Similarly the criteria for
water readings to be taken immediately recognises that a small
sample of water left in the sun quickly escalates in
temperature and that a thermometer kept on a hook in the sun takes time to reflect the ambient
temperature of the
water (
of course some buckets eventually contained an integral thermometer)
Tung and co-author Xianyao Chen
of the Ocean University
of China, who was a UW visiting professor last year, used recent observations
of deep - sea
temperatures from Argo floats that
sample the
water down to 6,500 feet (2,000 meters) depth.
Well, I was one
of the first persons in the blogosphere at the time to evaluate that, because I compared the dip in the
temperature of sampled water with the dip in the
temperature of near - surface air measured on ships, and observed that approximately half or so
of the dip was explainable by instrumentation changes and the remainder by some other mechanism — probably a change in internal ocean dynamics (PDO, AMO, etc..)
Due to the high specific heat
of water one needs to supply the
water sample with more energy in order to rise the
temperature by one degree than in the case
of some other material with the same mass but the lower heat capacity.
Relative humidity reflects the ratio
of the actual pressure
of water vapor in a
sample of air to the pressure necessary to saturate that air at a given
temperature.
From the press release: «During field expeditions, the research team used a variety
of techniques — including sonar and visual images
of methane bubbles in the
water, air and
water sampling, seafloor drilling and
temperature readings — to determine the conditions
of the
water and permafrost, as well as the amount
of methane being released.»
How do we know the
temperature change in the
water column on any given month in any particular body
of water unless systematic
sampling is being done which really only occured in the last 5 years with submersible probes?
Just to state that I was on a member
of a North sea survey crew back in the early 1980's when throwing a bucket over the side
of the ship was the accepted method
of obtaining
water samples for
temperature / salinity analysis.