Temperature Change Sample Clauses
The Temperature Change clause defines how parties will address and manage changes in temperature that may affect the performance or outcome of a contract. Typically, this clause outlines acceptable temperature ranges for work or product storage, and may specify procedures for notifying the other party if temperatures fall outside these limits. By establishing clear guidelines for temperature-related contingencies, the clause helps prevent disputes and ensures that both parties understand their responsibilities in maintaining suitable conditions.
Temperature Change. We will pay for loss to covered personal property in a building structure at the residence premises resulting from a change in temperature. The change in temperature must result from a covered loss to the building structure. This coverage does not increase the limit of liability applying to the damaged property.
Temperature Change. (Range): 120 deg F (67 deg C), ambient; 180 deg F (100 deg C), material surfaces.
Temperature Change. Temperatures in Bhutan are rising and expected to continue. Observations show that annual average temperatures have been increasing between 1996 and 2018. This is reflected in increases in mean and maximum daily temperatures, as well as decreases in minimum daily temperatures (see Annex II: Feasibility Study). Downscaled future projections from a validated set of 6 NASA NEX-GDDP models, consistent with projections in the SNC, project higher temperature increases in winter, similar to those for Southeast Asia from ensemble model simulations presented in both the Fourth (AR4) and Fifth (FAR) Assessment Report of the IPCC. Under RCP4.5 an increase of 0.8°C – 2.8°C during 2021-2100 is simulated, whereas under RCP8.5 an increase of between 0.8°C to more than 3.2°C is simulated towards the end of the century. All models show a progressive and steady increase in air temperature from 1980 to 2100, with concomitant increases in temperature extremes, as seen so far in observations. 24. Regional temperature projections indicate that average annual temperatures will rise by more than 2°C in South Asia by the mid-21st century and exceed 3°C by the late-21st century under a high-emissions scenario, compared to the 20th century, with the highest daily maximum temperatures potentially increasing by 4-5°C. IPCC’s 5th Assessment states that over the mid-term (2046–2065), an increase of 2-4°C is projected for the south Asian region with the warmest temperatures concentrated in amongst others Bhutan. Mean annual temperature in Bhutan is expected to increase by 0.8-1.0°C before 2039 and by 2.0-2.4°C before 2069. 25. Rainfall change: Annual rainfall over Bhutan is highly variable, with nearly all 17 class A stations demonstrating an average downward trend in both winter and monsoonal rainfall between 1996 and 2018 (see Annex II: Feasibility Study). Total rainfall at stations is often dependent on their altitude. CRU data confirm this decline in rainfall over the longer-term (1970-2014). This reduction in rainfall is further reflected in negative trends (reductions) in snow areas between 2002- 2010 suggesting that similar processes may be responsible for reductions at higher altitudes. 26. Negative trends in rainfall and effective rainfall are prevalent during winter, spring and summer at mid to high altitudes, which importantly are the source regions of the main rivers and streams. These trends are critical in terms of water GREEN CLIMATE FUND FUNDING PROPOSAL | PAGE 10 OF 73
Temperature Change. P L
Section I Conditions