Snowpack example sentences

"Snowpack" Example Sentences

1. A deep snowpack ensured an ample supply of water for the coming irrigation season.
2. The heavy snowfall resulted in an above average snowpack for that time of year.
3. Mountaineers carefully monitored the snowpack conditions before attempting ascents of high peaks.
4. Avalanche warnings were issued due to unstable conditions in the snowpack.
5. The below average winter snowfall left the mountain snowpack at dangerously low levels.
6. Forecasters tracked changes in the snowpack depth and density throughout the winter months.
7. Water managers measured the snowpack to predict spring river flows.
8. Warm spells in winter can melt significant portions of the snowpack.
9. The deep and stable snowpack allowed for backcountry skiing throughout most of the season.
10. Snowpack surveys provide important data to help monitor water availability.
11. Early melt-off of the snowpack can lead to flooding and problems with erosion.
12. The built up snowpack from successive storms created an avalanche hazard.
13. The high water content of a deep snowpack feeds streams and rivers long after snow has fallen.
14. The snowpack stabilizes as layers within the pack settle and bond together over time.
15. The late season snowfall added critical depth to the depleted winter snowpack.
16. Foresters relied on the stability of the snowpack to minimize fire risks during shut down periods.
17. An unusually dense snowpack resulted from changes in winter weather patterns.
18. The winter snowpack melted more slowly in shaded, north facing locations.
19. The deep and consistent snowpack provided a smooth ride on cross country skis.
20. Warmer temperatures shortened the duration of the annual snowpack.
21. An unusually thick snowpack formed on mountain ridges that winter.
22. Cold weather kept the snowpack intact well into the spring season that year.
23. The depth and condition of the mountain snowpack determined the longevity of the ski season.
24. Protracted cold snaps hardened and compacted the fragile winter snowpack.
25. Parks officials closed trails when unstable conditions developed within the snowpack.
26. The deep snowpack provided steady stream flows and filled reservoirs beyond capacity.
27. Significant settlement had occurred within the mountain snowpack by midwinter.
28. The dry winter left very little snowpack upon which spring wildflowers could draw moisture.
29. Steep east facing slopes kept less snowpack than more gently sloping western exposures.
30. Rangers warned of an increased avalanche risk due to unstable layers forming within the snowpack.
31. The shallow snowpack consisted mainly of loose powdery flakes.
32. An early season melt cycle weakened layers within the developing snowpack.
33. Rain pounded the snowpack, loosening weaker layers and priming future slides.
34. Much of the snowpack melted by mid-spring after a warm and dry April.
35. The ideal snowpack conditions produced optimal spring skiing.
36. The dense snowpack provided insulation that helped save perennial crops from cold temperatures.
37. The Sierra snowpack largely determines water availability for Central Valley farms.
38. Scientists studied the snowpack to gain insights into climate change impacts.
39. An unusually thin snowpack worried water managers and farmers preparing for the next growing season.
40. Despite record snowfall, much of the snowpack sublimated before it could enter streams and reservoirs.
41. An aging snowpack became prone to slides and melt-outs as bonding layers weakened.
42. The gradual spring melt of the snowpack recharged aquifers and filled streams and ponds.
43. Snowpack surveys helped resource managers anticipate problems from low water levels.
44. The record setting snowpack produced major flooding upon spring thaw.
45. The heavy, wet snowpack collapsed several barn roofs under its weight.
46. An unusually shallow and unstable snowpack was a concern for backcountry skiers.
47. Changes in the timing and amount of snowpacks are troubling signs of climate instability.
48. The quality of the snowpack affects the intensity and duration of spring runoff.
49. Warming winter temperatures gradually depleted mountain snowpacks in recent years.
50. Thin snowpacks caused local water shortages and led to fire bans the following summer.
51. Early season snowfalls contribute disproportionately to total snowpack.
52. Scientists studied historical snowpack records to determine long term trends.
53. Rapid melting of the high mountain snowpack caused flash flooding in downstream valleys.
54. Heavy winter rains diminished what little accumulation had formed in the snowpack.
55. The slow, sustained melt of the seasonal snowpack provided maximum groundwater recharge.
56. The dissolution of the winter snowpack heralded the coming of spring.
57. Multi-year snowpacks develop in very cold climates where subzero temperatures persist.
58. Backcountry trekkers modified their routes based on snowpack conditions.
59. Hydrologists relied on snowpack data to plan for summer reservoir releases.
60. Years of below average snowpacks led to drought conditions and water restrictions.

Common Phases

1. The snowpack remained low throughout the winter, leading to drought concerns.
2. They monitored the snowpack levels in the mountains to predict water runoff in the spring.
3. The high snowpack at the start of spring caused snowmelt flooding along rivers and streams.
4. The abnormally large snowpack was weighing down trees and power lines.
5. The warm rain melted the thin snowpack quickly, causing flash flooding.
6. Snowpack measurements help determine the amount of water runoff for crops and reservoirs.
7. Avalanche activity increases during periods of rapid snowpack loading.
8. A lot of moisture in the high snowpack created ideal conditions for wildflower blooms.
9. Scientists studied the snowpack levels to predict wildfire risks in the upcoming summer.
10. The Forest Service maintained several monitoring stations throughout the mountain snowpack.
11. Snowpack telemetry data feeds into water supply forecasting models.
12. The low-density snowpack led to avalanche concerns throughout the winter backcountry season.
13. The deep snowpack posed challenges for wildlife trying to find food.
14. Warming trends tend to reduce the total snowpack accumulation each winter season.
15. The record high snowpack lasted well into the spring months.
16. Researchers use snowpack sensors to track key metrics like snow depth, water content and temperature.
17. Snowshoeing through the deep snowpack left me exhausted by the end of the hike.
18. The spring runoff depends greatly on the snowpack water content from winter storms.
19. Light and fluffy snow creates poor snowpack insulation for overwintering seedlings.
20. Researchers flew over the mountains to map snowpack distribution using lidar sensing.
21. The stable snowpack offered great skiing and riding conditions on the slopes.
22. The shallow snowpack prevented us from snowshoeing to our usual winter camping spots.
23. It was quite a struggle digging out from beneath the heavy snowpack after the blizzard.
24. Avalanche mitigation efforts often focus on controlling snowpack loading on susceptible slopes.
25. Spring hiking season had to be delayed due to deep and lingering snowpack at higher elevations.
26. Low winter temperatures produced highly structured snowpack layers all season long.
27. Fresh snowfall increased the instability of the weak snowpack.
28. Ultrasonic snowpack sensors can monitor different internal layers and densities.
29. The reduced snowpack lowered streamflows into the summer irrigation season.
30. The lack of insulating snowpack left crops vulnerable to late season freezes.
31. Hunters had to trek for miles above the thin snowpack to find game this season.
32. Cold, dry snow makes the most stable snowpack conditions.
33. We found plenty of evidence indicating avalanche activity within the broken snowpack.
34. Blowing snow drifts created uneven snowpack accumulation across the landscape.
35. Most rain on snow events produce unstable wet snowpack conditions.
36. Each winter creates a unique snowpack profile with different hazards and challenges.
37. Snowpack telemetry readings help predict natural hazard risks over the coming months.
38. Cold, dry winters maximize the potential usable snowpack water equivalent.
39. Increased solar radiation absorption during midwinter thaws alters snowpack stratigraphy.
40. The changing climate has disrupted historical patterns in snowpack accumulation and ablation.
41. Wet spring storms threatened to induce slide activity within the stressed snowpack.
42. The dense snowpack effectively blanketed early season weeds.
43. Backcountry travelers had to negotiate obstacles hidden beneath the snowpack.
44. Snow depth and water content were several standard measurements taken of the snowpack.
45. Longer duration snowpack buildup promotes soil frost development and damage.
46. Avalanches become increasingly likely as the age and moisture content of the snowpack increase.
47. The heavy snowpack collapsed several roofs and overburdened drainage systems.
48. Increasing temperatures will reduce Sierra Nevada snowpack by 50% or more by 2100.
49. Logging operations ceased once snowpack accumulation became excessive on forest roads.
50. Low-elevation snowpack typically melts out much earlier in the spring.
51. The compressive forces within the deep snowpack eventually cracked bedrock and concrete foundations.
52. Mountain pine beetle relied on a deep snowpack to survive winter conditions.
53. Forest management strategies must adapt to significant decreases in winter snowpack.
54. Wind tends to redistribute surface snowpack into drifts and exposed areas.
55. Thawing then re-freezing creates ice lenses within the lower layers of the snowpack.
56. The historical record surrounding snowpack variability is crucial to future water management.
57. Years with poor snowpack accumulation often portend crop failures and wildfires.
58. Continuous snowpack depth measurements enhance forecasts of flood risk and water supply availability.
59. Snowpack sensors helped warn of avalanche potential and other dangers.
60. Storm season totals pale in comparison to seasonal snowpack accumulation.