Sentences with phrase «feedback cycle times»

But I'm optimistic about the potential of unbundling the role of the teacher and leveraging technology to create an online system for measuring and tracking student learning growth that has the rigor of human - graded assessment, the advantage of quick feedback cycle times, and the validity and reliability that come from standardization.

Not exact matches

«The world isn't really on an annual cycle anymore,» GE head of human resources Susan Peters said at the time, explaining that millennial workers in particular wanted faster, more frequent, mobile - enabled feedback.

For in - house recruiters, the ability to share applicant information with the relevant hiring manager, as well as schedule interviews and gather feedback from those same hiring managers within one system can save time and decrease the number of days in the hiring cycle.

To achieve long - term improvement of a skill, it's a good idea to move through this cycle of training - practice - feedback several times over several months.

PER and TIM block the ability of CLOCK to turn on these genes at the same time as they are producing the oscillations of the central feedback loop — setting up extended patterns of cycling gene activity.

This means that (1) animals are directly involved in an oxygen - regulating cycle or feedback loop that has previously been overlooked, and (2) we can directly test the idea (despite the uncertainties associated with looking so far back in time) by looking for a decrease in ocean oxygenation in conjunction with the spread of bioturbation.

For instance, the sensitivity only including the fast feedbacks (e.g. ignoring land ice and vegetation), or the sensitivity of a particular class of climate model (e.g. the «Charney sensitivity»), or the sensitivity of the whole system except the carbon cycle (the Earth System Sensitivity), or the transient sensitivity tied to a specific date or period of time (i.e. the Transient Climate Response (TCR) to 1 % increasing CO2 after 70 years).

If your cycles stay short after another month or two, then it may be time to talk about testing progesterone levels or getting your doctors feedback.

Cycle your feedback: It's tempting to spend enormous amounts of time commenting on student work.

The main areas covered in this work booklet are: The nervous system Reflexes Removing waste Synapses Reaction time The eye The brain Temperature regulation Water regulation Glucose regulation Negative feedback Menstrual cycle Contraception Fertility treatment Plant hormones Within the booklet are a range of different activities for students to work through to help them remember the content.

Specification points covered are: Paper 2 Topic 1 (4.5 - homeostasis and response) 4.5.1 - Homeostasis (B5.1 lesson) 4.5.3.2 - Control of blood glucose concentration (B5.1 lesson) 4.5.2.1 - Structure and function (B5.2 lesson) Required practical 7 - plan and carry out an investigation into the effect of a factor on human reaction time (B5.2 lesson) 4.5.3.1 - Human endocrine system (B5.6 lesson) 4.5.3.4 - Hormones in human reproduction (B5.10 lesson) 4.5.3.5 - Contraception (B5.11 lesson) 4.5.3.6 - The use of hormones to treat infertility (HT only)(B5.12 lesson) 4.5.3.7 - Negative feedback (HT only)(B5.13 lesson) Paper 2 topic 2 (4.6 - Inheritance, variation and evolution) 4.6.1.1 - sexual and asexual reproduction (B6.1 lesson) 4.6.1.2 - Meiosis (B6.1 lesson) 4.6.1.4 - DNA and the genome (B6.3 lesson) 4.6.1.6 - Genetic inheritance (B6.5 lesson) 4.6.1.7 - Inherited disorders (B6.6 lesson) 4.6.1.8 - Sex determination (B6.5 lesson) 4.6.2.1 - Variation (B6.9 lesson) 4.6.2.2 - Evolution (B6.10 lesson) 4.6.2.3 - Selective breeding (B6.11 lesson) 4.6.2.4 - Genetic engineering (B6.11 lesson) 4.6.3.4 - Evidence for evolution (B6.16 lesson) 4.6.3.5 - Fossils (B6.16 lesson) 4.6.3.6 - Extinction (B6.16 lesson) 4.6.3.7 - Resistant bacteria (B6.17 lesson) 4.6.4.1 - classification of living organisms (B6.18 lesson) Paper 2 topic 3 (4.7 - Ecology 4.7.1.1 - Communities (B7.1 lesson) 4.7.1.2 - Abiotic factors (B7.1 lesson) 4.7.1.3 - Biotic factors (B7.1 lesson) 4.7.1.4 — Adaptations (B7.2 lesson) 4.7.2.1 - Levels of organisation (feeding relationships + predator - prey cycles)(B7.3 lesson) 4.7.2.1 - Levels of organisation (required practical 9 - population sizes)(B7.4 lesson) 4.7.2.2 - How materials are cycled (B7.5 lesson) 4.7.3.1 - Biodiversity (B7.7 lesson) 4.7.3.6 - Maintaining Biodiversity (B7.7 lesson) 4.7.3.2 - Waste management (B7.9 lesson) 4.7.3.3 - Land use (B7.9 lesson) 4.7.3.4 - Deforestation (B7.9 lesson) 4.7.3.5 - Global warming (B7.9 lesson)

The candidate provides time and expectation for ELLs and staff to participate I multiple cycle of field testing, feedback and revision of the instructional program

During the fifth year of the cycle, district level feedback is gathered and at that point in time, recommendations are made to the State Board of Education to adjust, delete or add to academic standards.

AUSL's continuous improvement process is centered on ongoing cycles of real - time, data - driven, action - focused feedback and intervention.

These models do not include the major carbon cycle feedbacks, which only exacerbate the temperature rise, and bring potential extinction closer in time.

(57k) When I state that the equilibrium climatic response must balance imposed RF (and feedbacks that occur), I am referring to a global time average RF and global time average response (in terms of radiative and convective fluxes), on a time scale sufficient to characterize the climatic state (including cycles driven by externally - forced cycles (diurnal, annual) and internal variability.

Starting from an old equilbrium, a change in radiative forcing results in a radiative imbalance, which results in energy accumulation or depletion, which causes a temperature response that approahes equilibrium when the remaining imbalance approaches zero — thus the equilibrium climatic response, in the global - time average (for a time period long enough to characterize the climatic state, including externally imposed cycles (day, year) and internal variability), causes an opposite change in radiative fluxes (via Planck function)(plus convective fluxes, etc, where they occur) equal in magnitude to the sum of the (externally) imposed forcing plus any «forcings» caused by non-Planck feedbacks (in particular, climate - dependent changes in optical properties, + etc.).)

The equilbrium global time average response (on a time scale sufficient to characterize externally - forced cycles (day, year) and internal varibility) to an imposed global time average radiative forcing is a change that balances the externally imposed forcing plus any non-Planck feedbacks (where the Planck response is part of the response to the other feedbacks.

We are simply running out of time to stop all of the carbon cycle feedbacks from intensifying and to stop these devastating, record - breaking wildfires from becoming the normal climate.

The time period we have left at current emissions rates would be reduced by 6 years, to as little as 16 years, if we give ourselves a two - thirds chance of staying below two degrees, once we factor in carbon cycle feedbacks.

During that time natural cycles like the Milankovitch cycles, would trigger warming releasing CO2 resulting in a positive feedback.

Finally, we represent the climate — carbon - cycle feedback by adding an extra, temperature - dependent component to the total anthropogenic emissions emitted each year (Ea): where T ′ is the temperature anomaly above an exponentially weighted running mean with a time constant of 100 years, and b5 is the adjustable carbon - cycle feedback parameter.

BUT, other important / related parameters — BRDF (bidirectional reflectance distribution function)-- albedo i. /: 00 solar local time Neural network based on CYCLOPES and MODIS / wrong ALSO Need to make assumptions about carbon lost via respiration to go from GPP to / Cox et al. (2000) Acceleration of global warming due to carbon - cycle feedbacks in a coupled / / JRC / FastOpt: http://www.fastopt.com/topics/publications.htmlhttp://www.fastopt.com/topics/publications.html 50 0 = water; 1 /

But the «big climate picture» includes ocean feedbacks on all time scales, carbon and other elemental cycles, etc. and it has to be several decades before that is sorted out I would think.

Yesterday we saw that combining ocean thermal inertia, ocean carbon cycle inertia and climate sensitivity fast feedback inertia, there may still be a warming time lag of up to 10 years (the first years of which show rapid warming, beyond which we see progression to asymptote).

However, the timing, strength, and overall role of dust − climate feedbacks over these cycles remain unclear.

«Each of these subsystems has a host of known and unknown forcings, interactions, phase transitions, limitations, resonances, couplings, response times, feedbacks, natural cycles, emergent phenomena, constructal constraints, and control systems.

System energy forcings change all the time, on seconds to milenium time scales: sunshine, cloud overcast, day - night, summer — winter, monsoons, ENSO, PDO etc etc milankovitch cycles, Feedback is all about the while back in those cycles.

I don't think it could double the human impact, releasing as much carbon as we do, or else the natural world would be «tippier» than it is observed to be, with the occasional meltdown like the PETM but not meltdowns all the time, like models do if you set them up with a carbon cycle feedback that is too strong or acts too quickly.

AR4 missed the time frame for system changes that caused the Arctic sea ice retreat and all of the follow - on feedback cycles (e. g., CH4 releases from the Arctic sea bed).

«And it took us about 4 weeks to get that feedback cycle, so by the time that we got that feedback we had 4 more weeks of 100 % return rate that we'd shipped on top of that.»